Snowfall over central-eastern China and Asian atmospheric cold source in January
|
|
- Rudolph Watson
- 5 years ago
- Views:
Transcription
1 INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 32: (2012) Published online 21 March 2011 in Wiley Online Library (wileyonlinelibrary.com) DOI: /joc.2318 Snowfall over central-eastern China and Asian atmospheric cold source in January Sulan Nan a and Ping Zhao b,c * a Chinese Academy of Meteorological Sciences, Beijing, China b State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China c National Meteorological Information Centre, Beijing, China ABSTRACT: In January 2008, a severe snowstorm disaster occurred in central-eastern China. Using the monthly means from the National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) reanalysis data set and the observations from surface stations of China for the period , we statistically investigate the relationship between the January snowstorm weather over central-eastern China and the synchronous atmospheric thermal condition over the Asian continent. The results show that the extreme snowfall weather over central-eastern China is closely associated with the Asian atmospheric cold source (AACS) in January. When AACS is weak (corresponding to a higher AACS value), the heavy snowfall weather appears in central-eastern China. The values of both AACS and snowfall over central-eastern China in 2008 are most anomalous during the recent 30 years. This link may be explained by the atmospheric circulation well. Under a weak AACS (with a higher AACS value), a 500-mb anomalous low covers the mid-low latitudes of Asia, accompanying an anomalous high over the eastern coasts of East Asia. Accordingly, the southerly wind anomalies between the anomalous low and high prevail in the lower troposphere over central-eastern China, with the northerly wind anomalies prevail over this region at the surface, which also strengthen upward motion over central-eastern China. The southerly wind anomalies transport more water vapour into central-eastern China from both the South China Sea and the Bay of Bengal. These anomalies in the atmospheric circulation are responsible for the formation of the heavy snowfall weather in central-eastern China. Compared to both the El Niño-Southern Oscillation and Arctic Oscillation during winter, the thermal condition over the Asian continent has a closer relationship with the occurrence of the heavy snowfall weather over central-eastern China. Copyright 2011 Royal Meteorological Society KEY WORDS snowstorm over central-eastern China; Asian atmospheric cold source; East Asian winter monsoon Received 21 October 2009; Revised 9 December 2010; Accepted 10 February Introduction A severe snow disaster occurred in central-eastern China, North China, and the eastern part of Northwest China in January 2008, leading to the collapse of electric network and the severe damage of highway and railway transportation over these regions and an economic loss above billion Chinese Yuan. Therefore, many meteorologists have paid much attention to the causes for this disaster. Studying disastrous snowstorms has extensively received attention for a long term. Some progress has been made in understanding the links between snowstorm disasters and atmospheric circulation systems and the associated physical mechanisms. For example, the snowstorms occurring in North America and Europe are usually associated with the activities of fronts and cyclones at the mid latitudes of these regions (e.g. Braham, 1983; Ulbrich et al., 2001). Sanders (1986) investigated an effect of large-scale frontogenetical forcing and moist symmetric * Correspondence to: Ping Zhao, National Meteorological Information Centre, 46 Zhongguancun Nandajie, Beijing , China. zhaop@cma.gov.cn instability on a snowstorm process over the New England on 5 6 December Tayanç (1998) addressed that the blizzard over the eastern Mediterranean and Balkan regions in March 1987 may be related to the formation of the extensive blocking over northern Europe, the substantial amplification of the planetary-scale waves and the strong cyclogenesis over the eastern Mediterranean and Balkan region. Laird et al. (2003) emphasized the sensitivity of the lake-effect snowstorms in the United States to the local wind, temperature, moisture, and stability. Moreover, Ninomiya (1991) examined an effect of the development of a polar low near the eastern coast of the Asian continent to a Japanese snowstorm process on 9 11 December The persistent snowstorm weather often occurs under the background of a unique climate anomaly. Michanel and Smith (1994) pointed out that the blizzard occurring over the eastern part of the United States is related to El Niño-Southern Oscillation (ENSO). The winter atmospheric circulation in East Asia is characterized by the local strong lower-tropospheric northerly or northeasterly wind (e.g. Ramage, 1968; Chang et al., 1980), namely the East Asian winter monsoon (EAWM). Because the EAWM anomalies are related to atmospheric Copyright 2011 Royal Meteorological Society
2 SNOWFALL OVER CENTRAL-EASTERN CHINA AND ASIAN ATMOSPHERIC COLD SOURCE 889 intrinsic dynamic and thermal processes and external forcing, many studies paid attention to the EAWM circulation anomalies and the associated mechanisms. For example, the Arctic Oscillation (AO) may modulate EAWM through affecting the Siberian high (Wu and Wang, 2002). The EAWM anomalies are also usually accompanied by variations of upper-tropospheric westerly jet streams in the mid latitudes of Eurasia (Lau and Li, 1984; Zhang et al., 1997; Yang et al., 2002). When the propagation of quasi-stationary planetary waves into the stratosphere in the high latitudes of the Northern Hemisphere becomes weak, its propagation into the upper troposphere strengthens in the lower latitudes, which may lead to the weakening of the Siberian high and thus the weakening of the EAWM (Chen et al., 2008). Moreover, the land surface conditions on the mid-high latitudes of Eurasia and the tropical Pacific sea surface temperature (SST) anomalies are also related to the EAWM (Li, 1988; Chen and Sun, 2003). Snowstorms in eastern China often occur under the background of the EAWM circulation anomalies. Under such a background, low-level cold surges frequently invade into China along with the breakdown of the Siberia-Mongolia high (Tao, 1959). Shi et al. (2008) and Ji et al. (2008) showed that the snowstorm weather over central-eastern China in January 2008 was related to the strengthening of both the western Pacific subtropical high and India-Burma trough, and the southwesterly flow in front of the active India-Burma trough transports more moisture into central-eastern China, providing a favourable condition of water vapour for the occurrence of the snowstorm weather. Wen et al. (2009) investigated a link between this persistent snowstorm and jet stream anomalies over the Middle East. Hong and Li (2009) emphasized the combined effect of the intraseasonal oscillation heating over the Asian Maritime Continent and ENSO on initiating and maintaining the northerly anomaly over Southeast Asia in February after the snowstorm weather. In spite of the progress in understanding the EAWM variability and snowstorms over eastern China, some questions remain unanswered. For example, LaSW (2008) indicated that SST in the equatorial eastern Pacific and the AO might be the important factors influencing the persistent snowstorm over central-eastern China in January However, Gu et al. (2008) showed that the occurrence of this snowstorm disaster could not well be explained by the La Niña event. Moreover, Yang and Li (2008) addressed that the AO is also not closely related to this snowstorm weather. These results imply some differences in understanding the mechanism responsible for the formation of the January snowstorm weather over central-eastern China. Because the Asian atmospheric circulation anomalies are closely related to atmospheric thermal conditions over the Asian continent (Ye and Gao, 1979; Li and Yanai, 1996; Wu et al., 1997) and the EAWM intensity is modulated by the heating gradient between the Siberian region and the equatorial western Pacific (Ramage, 1968; Chang et al., 1980; Ding and Krishnamurti, 1987), some studies examined relationships between the Asian atmospheric thermal condition and the EAWM. For example, Zhao and Chen (2001) investigated relationships between the Tibetan winter cold source and the atmospheric circulation over the Asian-Pacific region. They addressed that during a weaker winter Asian cold source, a 500-mb anomalous cyclonic circulation usually appears in the mid-low latitudes of Asia and there is a stronger India- Burma trough. This anomalous pattern in atmospheric circulation is similar to that associated with the persistent snowstorm over central-eastern China in January Moreover, Bao et al. (2010) investigated a relationship between the Tibetan Plateau climate and this extreme snowstorm event with an atmospheric general circulation model. They concluded that a warmer Tibetan Plateau (TP) provided a favourable atmospheric circulation condition for the occurrence of this snowstorm. Then, does a change in the Asian thermal condition affect the snowstorm disaster over central-eastern China? If yes, what physical processes are responsible for the formation of the snowstorm weather? With these questions in mind, the objective of this work is therefore to investigate relationships of the atmospheric thermal condition over the Asian continent with the snowfall weather over central-eastern China during January and the associated physical processes. The rest of this article is organized as follows. In Section 2, we describe the main features of data sets and analysis methods. In Section 3, we study variability of the extreme snowfall over central-eastern China and analyse its relationships with the atmospheric cold source over Asia. Finally, conclusions and discussions are provided in Section Data and methods We utilize observations of the number of snowfall days (NSDs) at 527 surface stations in China (Figure 1(a)) from the National Meteorological Information Centre of China Meteorological Administration and the monthly data from the NCEP-NCAR reanalysis (Kalnay et al., 1996) for the period The monthly mean SST from the HadISST data set (Rayner et al., 2003) with a horizontal resolution of 1 in latitude and longitude is also used in this study. The AO index is from the Climate Prediction Center of NOAA s National Weather Service. To increase the reliability of our results obtained using the NCEP-NCAR reanalysis, we repeated some analyses using the monthly data from the European Centre for Medium-Range Weather Forecast (ECMWF) ERA-40 data set for (Uppala et al., 2005). Following the previous study (Yanai et al., 1992; Zhao and Chen, 2001), for an air column, the atmospheric apparent heat source/sink (<Q 1 >)isdefinedas <Q 1 >= SH + R net + LP
3 890 S. NAN AND P. ZHAO (a) is used to assess the statistical significance. Unless specified, the 90% confidence level is used to measure a significant signal. (b) Figure 1. (a) Distribution of surface meteorological stations in China, in which the small box indicates central-eastern China ( E/ N). (b) The anomaly of NSD (unit: day) in January 2008 from the climatology ( ). In (b), the shaded areas are 9days. where SH is the sensible heat flux at surface, R net the net radiation absorbed by the air column, and LH the latent heat produced by precipitation condensation. Because <Q 1 > is usually negative in winter in continents, the atmosphere shows a cold-source feature, which is called the atmospheric cold source (Yanai et al., 1992; Zhao and Chen, 2001). In this study, we use the downward shortwave radiation flux, the upward longwave radiation flux, the upward solar radiation flux at tropopause, the SH, the net longwave radiation, the net shortwave radiation at the surface, and the precipitation rate from the NCEP reanalysis data set to calculate <Q 1 >. Moreover, the surface thermal radiation, the surface solar radiation, the top solar radiation, the top thermal radiation, the surface sensible heat flux, the convective precipitation, and the stratiform precipitation (large-scale precipitation) from the ERA-40 reanalysis data set are also used to calculate <Q 1 >. The analysis methods employed in this study include correlation and composite analyses. The Student s t-test 3. Relationship between snowfall over central-eastern China and Asian atmospheric heating 3.1. Snowfall and associated atmospheric circulation and heating in January 2008 It is necessary to briefly review the snowfall weather over central-eastern China in January 2008 and the associated atmospheric circulation and atmospheric cold source before studying the climatological features of the snowfall weather over central-eastern China and associated physical processes during Because NSD may reflect both precipitation and temperature information, we select NSD as an indicator of the snowstorm weather. Figure 1(b) is the anomaly of NSD in January 2008 from the climatological ( ) mean value. Positive NSD values cover the region to the south of 40 N (including central-eastern China, North China, and the eastern part of Northwest China) and the large-scale NSD value exceeding 9 days mainly appears over centraleastern China (east of 105 E) between 25 N and 35 N, with the central value of 12 days in the middle and lower valleys of the Yangtze River. It is evident that NSD over these regions is much bigger in January 2008 than its climatological mean value. Moreover, some scatted centres of 9 days also appear over northwestern China (north of 35 N and west of 105 E). The anomaly of atmospheric circulation directly caused this snowstorm weather in Figure 2(a) shows the climatology of 500-mb geopotential height during and the anomaly of the 500-mb height in January 2008 from the climatology. In the figure, there was a large-scale anomalous low at the mid-low latitudes of the Asian continent. Because an extratropical ridge appears over Asia on the climatological map, this anomalous low indicates a weaker ridge in the mid-low latitudes of Asia during January To the north of the anomalous low, there were positive anomalies, indicating a weaker Arctic low over Eurasia. Meanwhile, positive anomalies also appeared over the eastern coasts of East Asia where the southern part of a long-wave trough over East Asia and the northern part of the western North Pacific subtropical ridge often appear, suggesting the weakening of the trough and the northwestward subtropical ridge relative to the climatology. Corresponding to the variations in the 500-mb height field at the mid-low latitudes of the Asian-western Pacific region, some pronounced changes are also observed in the lower troposphere and at the surface. At 850- mb (Figure 2(b)), negative geopotential height anomalies appeared over Asia to the south of 30 N, with their centres below 10 gpm, while positive geopotential height anomalies appeared over the eastern coasts of East Asia. In the wind field (Figure 2(b)), there was an anomalous cyclonic circulation around the TP, indicating a
4 SNOWFALL OVER CENTRAL-EASTERN CHINA AND ASIAN ATMOSPHERIC COLD SOURCE 891 Figure 2. (a) The climatology of January 500-mb geopotential height for (shade; unit: gpm) and the anomaly of January 500-mb geopotential height in 2008 (contour; unit: gpm) from the climatology. (b) The anomalies of January 850-mb geopotential height (shade; unit: gpm) and horizontal winds (vector; unit: m s 1 ) in (c) The anomalies of January surface wind (vector; unit: m s 1 ) and surface pressure (contour; unit: Pa) in In (b) and (c), the thick line is the 1500-m topographic contour. stronger India-Burma trough, and there was an anomalous anticyclone over the eastern coasts of East Asia, with its circulation centre appearing near 120 E/45 N. The anomalous southerly winds to the southwest of the anomalous anticyclone centre and from the Bay of Bengal prevailed over eastern China, transporting water vapour into central-eastern China. Corresponding to the positive anomalies of the 500- and 850-mb geopotential heights over the eastern coasts of East Asia, there existed a positive anomaly of surface pressure, with its centre appearing at 120 E/45 N (Figure 2(c)). To the south of the positive pressure anomalies, anomalous northerly or northeasterly winds prevailed over central-eastern China south of 40 N, which favoured the invasion of cold air masses into central-eastern China. This vertical structure with warm and wet air masses in the lower troposphere and the underlying cold masses was favourable for the persistent freezing rain and snowfall over central-eastern China. Then, what reasons may be responsible for the variations of the India-Burma trough and the trough over the eastern coasts of East Asia? Following the previous studies (Ramage, 1968; Chang et al., 1980; Zhao and Chen, 2001), we examine the atmospheric thermal condition over the Asian continent. Figure 3 shows the anomaly of <Q 1 > in January Positive anomalies of <Q 1 > covered
5 892 S. NAN AND P. ZHAO most of the Asian hinterland between 20 N and 50 N and between 80 E and 100 E, with the centres of 150 W m 2 near 97.5 E/ N, 100 W m 2 near E/40 N and 65 E/32.5 N, and 200 W m 2 near 75 E/ N, indicating a weaker atmospheric cold source over these regions relative to the climatological mean value. Then, does this relationship of the extreme snowfall weather over central-eastern China with the atmospheric circulations in the mid-low latitudes of the Asian-Pacific region and <Q 1 > over the Asian continent occur in the other years? In the following section, we expand the above analyses to the period Variations of snowfall over central-eastern China and Asian atmospheric heating Figure 4(a) shows the standard deviation of <Q 1 > during Over the Asian continent, the standard deviation of <Q 1 > exceeding 60 W m 2 appears in the region E/25 50 N. These features are also observed from the result of the ERA-40 reanalysis (shown in Section 4). Comparing with Figure 3, it is seen that the Asian positive anomalies of <Q 1 > in January 2008 correspond to the large standard deviation of <Q 1 >. Referring to the distributions of the Asian large standard deviation shown in Figure 4(a) and <Q 1 > in January 2008 shown in Figure 3, the regionally ( E/25 50 N) averaged <Q 1 > is defined as the Asian atmospheric cold source (AACS) index in January. Figure 4(b) shows the correlation between the January AACS index and the simultaneous <Q 1 > at each grid point during It appears that the significant positive correlation covers a broad area in the middle latitudes from the Mediterranean Sea to East Asia, with a maximum correlation coefficient of 0.6 appearing between 30 N and 40 N. Clearly, the AACS index well represents the variability of AACS at the mid-low latitudes of the Asian continent. More calculation shows that the temporally averaged value of the AACS index over is 80.6 Wm 2, with a standard deviation of 10.8 W m 2. Figure 5(a) shows the time series of the normalized January AACS index. In the figure, the Figure 3. The anomaly of January <Q 1 > (unit: W m 2 ) in 2008 from the climatology ( ). Figure 4. (a) The standard deviation of January <Q 1 > (unit: Wm 2 ) during , in which the contours 5, 15, 30, 50, 80, and 120 W m 2 are plotted and the box indicates the region ( E/25 50 N) defining the AACS index. (b) Correlation coefficient between the January AACS index and the synchronous <Q 1 > at each grid point during , in which the light and heavy shaded areas are significant at the 90% confidence level for the negative and positive values, respectively. AACS index exhibits the remarkable interannual variability, with the biggest value of 50.4 W m 2 in 1969 and the smallest value of W m 2 in In 2008, this index is most anomalous during the recent 30 years. Referring to the position of the large NSD value exceeding 9 days over central-eastern China in January 2008, we use the regionally averaged NSD value over E/25 35 N (including 177 stations in Figure 1(a)) as an index of NSD over central-eastern China (hereafter referred to as the NSD-CEC index). Figure 5(b) shows the time series of the January normalized NSD-CEC index. The climatological ( ) mean value of the NSD-CEC index is 4.3 days, with its standard deviation of 2.1 days. The January NSD-CEC index also exhibits the remarkably interannual variability, with the biggest value of 11.2 days in 1977 and the smallest value of 1.2 days in In 2008, the NSD- CEC is also most anomalous during the recent 30 years. A correlation analysis shows that the correlation coefficient between the AACS and NSD-CEC indices is 0.56
6 SNOWFALL OVER CENTRAL-EASTERN CHINA AND ASIAN ATMOSPHERIC COLD SOURCE 893 Figure 5. Time series of the normalized AACS index from the NCEP-NCAR reanalysis (a) and the normalized NSD-CEC index for (b). for the period (significantly at the 99.9% confidence level), greater than those between the AACS index and the synchronous precipitation (0.38, significant at the 99% confidence level) over central-eastern China ( E/25 35 N) and between the AACS index and the synchronous temperature ( 0.32, significant at the 98% confidence level). Although the formation of snowfall is greatly affected by both more water vapour and lower air temperature, snowfall is not equivalent to precipitation or air temperature. For example, when more (less) water vapour is accompanied by higher (lower) air temperature, it is difficult to form snowfall. To assess the robustness of the link between snowfall over centraleastern China and AACS, we slightly adjusted the regions where the NSD-CEC and AACS indices are defined, respectively. The results show that the time curves of these two indices do not show a substantial change, which suggests the robustness of this link. Moreover, in the seven highest NSD-CEC-index years (1956, 1969, 1974, 1977, 1984, 1993, and 2008) with their normalized values greater than one standard deviation, there are five years (1956, 1969, 1974, 1977, and 2008) with a positive anomaly of the AACS index (Table I). In the nine low NSD-CEC-index years (1963, 1965, 1975, 1986, 1987, 1992, 1999, 2002, and 2007) with their values less than one negative standard deviation, there are seven years (1963, 1975, 1986, 1987, 1992, 2002, and 2007) with a negative anomaly of the AACS index. These results further support a close relationship between AACS and the extreme snowfall weather over central-eastern China in January Snowfall over central-eastern China and East Asian atmospheric circulation associated with AACS To detect variations in the atmospheric circulation associated with the interannual variability of the January AACS Table I. Years with the extreme high and low normalized January NSD-CEC indices beyond one standard deviation (σ ) during and the corresponding normalized AACS, Niño 3 4 SST and AO indices during January. Years NSD-CEC AACS Niño 3.4 SST AO NSD-CEC σ NSD-CEC σ from a composite analysis, we select nine high and low AACS-index years on the basis of the January AACS index (displayed in Figure 5(a)). They are 1953, 1954, 1957, 1969, 1970, 1972, 1973, 1977, and 2008 for the high AACS-index years, called the high AACS-index cases, and 1963, 1976, 1979, 1982, 1986, 1987, 1990, 2003, and 2007 for the low AACS-index years, called the low AACS-index cases. The composite patterns of NSD in the high and low AACS-index cases are constructed (Figure 6). In general, the patterns in the high and low AACS-index cases
7 894 S. NAN AND P. ZHAO Figure 6. (a) The composite patterns of NSD (unit: day) for the high AACS-index cases. (b) Same as in (a), but for low AACS-index cases. (c) Same as in (a), but for the difference between (a) and (b), in which the shaded areas are at the 90% confidence level. are similar to that of the climatological mean. However, for the high AACS-index cases (Figure 6(a)), the NSD exceeding 6 days dominates most of central-eastern China (east of 100 E) between 25 N and 35 N, with the central value exceeding 9 days along the middle and lower valleys of the Yangtze River. For the low AACSindex cases (Figure 6(b)), NSD decreases remarkably. The NSD around 3 days dominates most of centraleastern China between 25 N and 35 N. Furthermore, the differences in NSD between the high and low AACSindex cases are greater than 4 days over the Yangtze River and Yellow River valleys, with a maximum difference of 8 days (Figure 6(c)). It is evident that when the AACS index is higher (lower), NSD is remarkably greater (smaller) over most of central-eastern China. Figure 7(a) shows the composite difference of 500-mb geopotential height between the high and low AACSindex cases. In the figure, negative anomalies below 60 gpm appear over Eurasia to the south of 50 N, indicating a weaker ridge at the mid-low latitudes of Asia on the climatological mean map, while the positive height anomalies appear in the high latitudes and Arctic region of Europe. Meanwhile, the positive anomalies also appear over the eastern coasts of East Asia, indicating the weakening of the East Asian long-wave trough and the northwestward subtropical western Pacific ridge relative to the climatology. Corresponding to the changes of 500-mb geopotential height over the Asian-western Pacific, in the 850-mb horizontal wind field (Figure 7(b)), an anomalous cyclonic circulation surrounds TP, while an anomalous anticyclone appears over Northeast Asia. Accordingly, the anomalous southwesterly to the southeast of the anomalous cyclonic circulation in the midlow latitudes of Asia and the southeasterly winds to the southwest of the anomalous anticyclonic circulation over Northeast Asia prevail over the mid-low latitudes of East Asia. At the surface (Figure 7(c)), anomalous northeasterly winds to the south of the anomalous anticyclonic circulation over Northeast Asia prevail over central-eastern China to the south of 40 N. These anomalous features of the atmospheric circulation between the high and low AACS-index cases favours the formation of the persistent snowstorm weather over central-eastern China, similar to those in January 2008 (shown in Figure 2). This similarity shows that the relationship among the extreme snowfall weather over central-eastern China, the atmospheric circulations over the Asian-Pacific region, and <Q 1 > over the Asian continent in 2008 does occur in the other years. Figure 8(a) further shows the composite difference in the integrated water vapour flux from the surface to 600-mb between the high and low AACS-index cases. It appears that the strong anomalous water vapour flux towards central-eastern China comes mainly from two passages. One originates from the South China Sea and then flows into central-eastern China. The other comes from the Bay of Bengal, and the southwesterly wind anomalies in front of the strengthened Indian- Burma trough (in Figure 7) transport more water vapour from the Bay of Bengal into eastern China. Figure 8(b) further shows the composite difference in the water vapour flux divergence between the high and low AACSindex cases. In the figure, central-eastern China to
8 SNOWFALL OVER CENTRAL-EASTERN CHINA AND ASIAN ATMOSPHERIC COLD SOURCE 895 Figure 7. (a) Composite differences of 500-mb geopotential height (unit: gpm) between the high and low AACS-index cases. (b) Same as in (a), but for 850-mb horizontal winds (unit: m s 1 ). (c) Same as in (a), but for surface wind (vector; unit: m s 1 ) and surface pressure (contour and shade; unit: Pa). In (a) and (c), the light and heavy shaded areas are significant at the 90% confidence level for negative and positive differences, respectively. the south of 40 N is covered by negative anomalies of the divergence, with the centre of 80 g cm 2 s 1 near E/25 N, indicating the enhanced convergence or reduced divergence of the water vapour flux in the lower troposphere over central-eastern China under a high AACS-index condition and vice versa. These strengthened transports of water vapour towards centraleastern China provide a favourable condition for the local heavy snowfall. Figure 9 shows the composite difference of vertical p-velocity along N. It is seen from the figure that significant negative anomalies appear to the east of 105 E, with a maximum magnitude of Pa s 1, indicating the strengthening of upward motion or the weakening of downward motion under a higher AACS-index condition. Thus, when the AACS index is higher, a variation in the atmospheric circulation over East Asia may strengthen upward motion or weaken downward motion over central-eastern China, favouring an increase in the local snowfall. In brief, AACS is closely related to the anomalous Asian atmospheric circulations. When the AACS index is higher, the 500-mb ridge at the mid-low latitudes of Asia is weaker, with a large-scale anomalous low over these regions, while the East Asian long-wave trough weakens and the subtropical high over the western North Pacific moves northwestward, with an anomalous high over the eastern coasts of East Asia. Accordingly, lower tropospheric anomalous southwesterly or southeasterly winds between the
9 896 S. NAN AND P. ZHAO Figure 8. Composite differences of water vapour flux (a; unit: 10 5 gcm 1 s 1 ) in the lower troposphere (from the surface to 600 mb) and its divergence (b; unit: 10 g cm 2 s 1 ) between the high and low AACS-index cases. The shaded areas are significant at the 90% confidence level. 4. Conclusions and discussions Figure 9. Longitude-height cross section of composite difference of vertical p-velocity (unit: 10 2 Pa s 1 ) along N between the high and low AACS-index cases. The light and heavy shaded areas are significant at the 90% confidence level for negative and positive differences, respectively. The black shaded area is for the topography. anomalous low and high prevail over eastern China with underlying anomalous northerly winds prevailing over the region, which strengthens the tropospheric upward motion over central-eastern China and the transport of low-level water vapour towards centraleastern China. These anomalies finally contribute to the occurrence of snowstorm weather over central-eastern China. Using the monthly mean NCEP-NCAR reanalysis data set and the monthly temperature, precipitation, and snowfall data from surface stations of China for the period , we have investigated the features of snowfall weather over central-eastern China, the atmospheric circulation over Asia-Pacific region, and the atmospheric cold source over the Asian continent in January 2008 and also examined the relationship between the January AACS and the synchronous snowfall over central-eastern China for the period The result shows that in January 2008, a severe snowstorm disaster occurred in central-eastern China and the NSDs over the region (NSD-CEC) were much bigger compared to the climatology. Meanwhile, AACS is much weak (with a high AACS-index value) relative to the climatology. Both the AACS and NSD-CEC in January 2008 are most anomalous during the recent 30 years. This relationship between the AACS and NSD-CEC is also observed for the period and there is a significantly positive correlation between AACS and NSD-CEC, namely that when the AACS index is higher (lower), the NSD value over central-eastern China is bigger (smaller). When AACS is weak, a 500-mb anomalous low covers the mid-low latitudes of Asia, accompanying an anomalous high over Northeast Asia. Under such an anomalous circulation pattern, anomalous southerly winds prevail in the lower troposphere over East Asia, while anomalous
10 SNOWFALL OVER CENTRAL-EASTERN CHINA AND ASIAN ATMOSPHERIC COLD SOURCE 897 (a) (b) Figure 10. (a) and (b) are same as in Figures 4a and 5a, respectively, but from the ERA-40 reanalysis. The shaded areas are 15 W m 2. northerly winds prevail at the surface over eastern China. This vertical feature of the anomalous atmospheric circulations is responsible for the persistent snowfall over central-eastern China. The anomalous southerly winds also favour the transports of water vapour towards eastern China from the South China Sea and the Bay of Bengal. Meanwhile, the anomalous upward motion occurs over central-eastern China. Thus, these atmospheric circulation anomalies provide a large-scale atmospheric circulation background and a favourable vapour condition for more snowfall over central-eastern China. Moreover, the atmospheric circulation anomalies associated with a higher AACS index are also consistent with those in January Therefore, the AACS index may be used as an indicator of the extremely heavy snowfall weather over central-eastern China. To verify the relationship between AACS and snowfall over central-eastern China and increase the reliability of the results obtained from the NCEP-NCAR reanalysis, we use the ERA-40 reanalysis data to repeat the above analyses. Figure 10(a) shows the standard deviation of <Q 1 > from the ERA-40 reanalysis. It is seen that high values exceeding 15 W m 2 occur over West Asia and South Asia. Although the standard deviation of <Q 1 > in the ERA-40 data is generally less than that in the NCEP-NCAR data, their distribution patterns are similar. In the same way, the AACS index is also calculated using the ERA-40 data (Figure 10(b)). There is a significant positive correlation of 0.69 between the NCEP-NCAR and ERA-40 <Q 1 > values. For the high AACS-index cases (1969, 1972, 1973, 1974, 1977, and 1991) from the ERA-40 data, NSD exceeding 9 days dominates central-eastern China (Figure 11(a)), while for the low AACS-index cases (1959, 1960, 1963, 1966, 1986, and 1987), NSD around 3 days appears over central-eastern China (Figure 11(b)). Compared to the low AACS-index cases, there are more snowfall days over central-eastern China in the high AACS-index cases (Figure 11(c)). These anomalous features are consistent with those from the NCEP-NCAR reanalysis (shown in Figure 6(c)). Figure 12(a) shows the composite difference of 500- mb geopotential height between the high and low ERA-40 AACS-index cases. In the figure, an anomalous low/an anomalous high appear over the mid-low latitudes of Asia/the eastern coasts of East Asia, indicating a weaker ridge over mid-low latitudes of Asia/a northwestward subtropical high over the western North Pacific and a weak East Asian long-wave trough. In the lower troposphere, anomalous southerly winds prevail over eastern China (Figure 12(b)). These results are also consistent with those from the NCEP-NCAR reanalysis, further increasing the reliability of out results. As mentioned in Section 1, the effects of ENSO and AO on the snowstorm weather are still an open question (e.g. Gu et al., 2008; LaSW, 2008; Yang and Li, 2008). Is snowfall over central-eastern China associated with ENSO and AO during ? Table I shows the
11 898 S. NAN AND P. ZHAO Figure 11. Same as in Figure 6, but for the AACS-index cases from the ERA-40 reanalysis. Figure 12. (a) and (b) are same as in Figure 7(a) and (b), respectively, but from the ERA-40 reanalysis. years with the extremely high or low January NSD-CEC index beyond one standard deviation during , the corresponding normalized SST index over the Niño 3 4 region ( W/5 S 5 N) used to indicate variability of ENSO and the corresponding normalized AO index. In seven years with a high NSD-CEC index, there are four years with a La Niña phase and four years with a positive AO index. In nine years with a low NSD- CEC index, there are six years with a La Niña phase and five years with a positive AO index. Although the heaviest snowstorm occurred over central-eastern China in both 1977 and 2008, there is an opposite sign in the Niño 3 4 or AO index between these two years. This weak relationship of the NSD-CEC index with the Niño
12 SNOWFALL OVER CENTRAL-EASTERN CHINA AND ASIAN ATMOSPHERIC COLD SOURCE or AO index is also supported by a correlation analysis. The correlation coefficient is 0.13 between the NSD-CEC and Niño 3 4 indices during and 0.03 between the NSD-CEC and AO indices, not significant at the 90% confidence level. These results imply that compared with the AACS index, the ENSO and AO indices are weaker in reflecting the variability of the January snowfall weather over central-eastern China. Acknowledgements We thank the Climate Diagnostic Center/NOAA for providing the NCEP-NCAR reanalysis data and UK Meteorological Office, Hadley Centre, for providing monthly mean HadISST data on their homepages. We also thank the Climate Prediction Center in NOAA/National Weather Service for providing AO index. The ECMWF ERA-40 data used in this study are obtained from the ECMWF data server. The work was jointly sponsored by the National Key Basic Research Project of China (2009CB421404), Basic Research Operation Foundation of Chinese Academy of Meteorological Sciences (2010Z003), and the National Natural Science Foundation of China ( ). References Bao Q, Yang J, Liu YM, Wu GX, Wang B Roles of anomalous Tibetan Plateau warming on the severe 2008 winter storm in Central- Southern China. Monthly Weather Review 138: Braham BR The midwest snow storm of 8 11 December Monthly Weather Review 111: Chang CP, Erickson J, Lau KM Northeasterly cold surges and near-equatorial disturbances over the winter-monex area during Part II: Planetary scale aspects. Monthly Weather Review 108: Chen HS, Sun ZB The effects of Eurasian snow cover anomaly on winter atmospheric general circulation Part I. observational studies. Chinese Journal of Atmospheric Sciences 27(3): (in Chinese). Chen W, Gu L, Wei K, Huang RH Studies of the dynamic processes of East Asian monsoon system and the quasi-stationary planetary wave activities. Chinese Journal of Atmospheric Sciences 32(4): (in Chinese). Ding YH, Krishnamurti TN Heat budget of the Siberian high and the winter monsoon. Monthly Weather Review 115: Gu L, Wei K, Huang RH Severe disaster of blizzard, freezing rain and low temperature in January 2008 in China and its association with the anomalies of East Asian monsoon system. Climatic and Environmental Research 13(4): (in Chinese). Hong CC, Li T The extreme cold anomaly over Southeast Asia in February 2008: roles of ISO and ENSO. Journal of Climate 22: Ji LR, Bueh C, Shi N, Xie ZW On the medium-range process of the rainy, snowy and cold weather of South China in early 2008 Part III: Pressure trough over the Tibetan Plateau/Bay of Bengal. Climatic and Environmental Research 4: (in Chinese). Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Coauthors The NCEP/NCAR 40-year reanalysis project. Bulletin of the American Meteorological Society 77: Laird NF, Walsh JE, Kristovich DAR Model simulations examining the relation of lake-effect morphology to lake shape, wind direction and wind speed. Monthly Weather Review 131: LaSW (State Key Laboratory of Severe Weather)/Chinese Academy of Meteorological Sciences) Analysis about features and causes on extreme rain-snow-ice weather over southern China in January LaSW Science Report: (in Chinese). Lau KM, Li MT The monsoons of East Asia and its global associations a survey. Bulletin of the American Meteorological Society 65: Li C Frequent activities of strong are troughs in East Asia wintertime and occurrence of El Niño events. Science in China (Series B) 31(6): Li C, Yanai M The onset and interannual variability of the Asian summer monsoon in relation to land-sea thermal contrast. Journal of Climate 9: Michanel SH, Smith TM The global climate for March-May 1993, mature ENSO conditions persist and a blizzard blankets the Eastern United States. Journal of Climate 7: Ninomiya K Polar low development over the east coast of Asian continent on 9 11 December Journal of the Meteorological Society of Japan 69(6): Ramage CS Role of the maritime continent on the atmospheric circulation. Monthly Weather Review 96: Rayner NA, Parker DE, Horton EB, Folland CK, Alexander LV, Rowell DP, Kent EC, Kaplan A A global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. Journal of Geophysical Research 108(D14): 4407, DOI: /2002JD Sanders F Frontogenesis and symmetric stability in a major New England snowstorm. Monthly Weather Review 114: Shi N, Bueh C, Ji LR, Wang PX On the Medium-range process of the rainy, snowy and cold weather of South China in early Part II: Characteristics of the western Pacific subtropical high. Climatic and Environmental Research 4: (in Chinese). Tao SY Studies on East Asian cold waves in the recent ten years. Acta Meteorologica Sinica 3: (in Chinese). Tayanç M March 1987 cyclone (Blizzard) over the Eastern Mediterranean and Balkan Region associated with blocking. Monthly Weather Review 126: Ulbrich U, Fink AH, Klawa M, Pinto JG Three extreme storms over Europe in December Weather 56(3): Uppala SM, KÅllberg PW, Simmmons AJ, Andrae U, Bechtold VDC, Fiorino M, Gibson JK, Haseler J, Hernandez A, Kelly GAX, Onogi K, Saarinen S, Sokka N, Allan RP, Andersson E, Arpe K, Balmaseda MA, Beljaars ACM, Van De Berg L, Bidlot J, Bormann N, Caires S, Chevallier F, Dethof A, Dragosavac M, Fisher M, Fuentes M, Hagemann S, Hólm E, Hoskins BJ, Isaksen L, Janssen PAEM, Jenne R, McNally AP, Mahfouf JF, Morcrette JJ, Rayner NA, Saunders RW, Simon P, Sterl A, Trenberth KE, Untch A, Vasiljevic D, Viterbo P, Woollen J The ERA-40 re-analysis. Quarterly Journal of the Royal Meteorological Society 612: Wen M, Yang S, Kumar A, Zhang PQ An analysis of the largescale climate anomalies associated with the snowstorms affecting China in January Monthly Weather Review 137: Wu BY, Wang J Winter Arctic Oscillation, Siberian High and East Asian winter monsoon. Geophysical Research Letters 29(19): DOI: /2002GL Wu GX, Li WP, Guo H, Liu H, Xue JS, Wang ZZ Sensible heat-driven air pump (SHAP) over the Tibetan Plateau and Asian summer monsoon. Commemorating Collection for Zhao Jiuzhang. Science Press Beijing: (in Chinese). Yanai M, Li C, Song Z Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon. Journal of the Meteorological Society of Japan 70: Yang H, Li CH Influence of Arctic Oscillation on temperature and precipitation in winter. Climatic and Environmental Research 13(4): (in Chinese). Yang S, Lau KM, Kim KM Variations of the East Asian jet stream and Asian-Pacific-American winter climate anomalies. Journal of Climate 15: Ye DZ, Gao YX The Meteorology of the Qinghai-Xizang Plateau. Science Press: (in Chinese). Zhang Y, Sperber KR, Boyle JS Climatology and interannual variation of the East Asia winter monsoon: results from the NCEP NCAR reanalysis. Monthly Weather Review 125: Zhao P, Chen LX Interannual variability of atmospheric heat source/sink over the Qinghai Xizang (Tibetan) Plateau and its relation to circulation. Advances in Atmospheric Sciences 18(1):
Weakening relationship between East Asian winter monsoon and ENSO after mid-1970s
Article Progress of Projects Supported by NSFC Atmospheric Science doi: 10.1007/s11434-012-5285-x Weakening relationship between East Asian winter monsoon and ENSO after mid-1970s WANG HuiJun 1,2* & HE
More informationThe feature of atmospheric circulation in the extremely warm winter 2006/2007
The feature of atmospheric circulation in the extremely warm winter 2006/2007 Hiroshi Hasegawa 1, Yayoi Harada 1, Hiroshi Nakamigawa 1, Atsushi Goto 1 1 Climate Prediction Division, Japan Meteorological
More informationThe Interdecadal Variation of the Western Pacific Subtropical High as Measured by 500 hpa Eddy Geopotential Height
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2015, VOL. 8, NO. 6, 371 375 The Interdecadal Variation of the Western Pacific Subtropical High as Measured by 500 hpa Eddy Geopotential Height HUANG Yan-Yan and
More informationInfluences of the Pacific Decadal Oscillation on the East Asian Summer Monsoon in non-enso years
ATMOSPHERIC SCIENCE LETTERS Atmos. Sci. Let. 17: 115 1 (16) Published online 9 November 15 in Wiley Online Library (wileyonlinelibrary.com) DOI: 1.1/asl.634 Influences of the Pacific Decadal Oscillation
More informationThe increase of snowfall in Northeast China after the mid 1980s
Article Atmospheric Science doi: 10.1007/s11434-012-5508-1 The increase of snowfall in Northeast China after the mid 1980s WANG HuiJun 1,2* & HE ShengPing 1,2,3 1 Nansen-Zhu International Research Center,
More informationDecadal Anomalies of Winter Precipitation over Southern China in Association with El Niño and La Niña
NO.1 YUAN Yuan, LI Chongyin and YANG Song 91 Decadal Anomalies of Winter Precipitation over Southern China in Association with El Niño and La Niña YUAN Yuan 1 ( ), LI Chongyin 2,3 ( ), and YANG Song 4
More informationRespective impacts of the East Asian winter monsoon and ENSO on winter rainfall in China
Click Here for Full Article JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2009jd012502, 2010 Respective impacts of the East Asian winter monsoon and ENSO on winter rainfall in China Lian-Tong
More informationLong-Term Changes in Rainfall over Eastern China and Large-Scale Atmospheric Circulation Associated with Recent Global Warming
1544 J O U R N A L O F C L I M A T E VOLUME 23 Long-Term Changes in Rainfall over Eastern China and Large-Scale Atmospheric Circulation Associated with Recent Global Warming PING ZHAO National Meteorological
More informationImpact of Eurasian spring snow decrement on East Asian summer precipitation
Impact of Eurasian spring snow decrement on East Asian summer precipitation Renhe Zhang 1,2 Ruonan Zhang 2 Zhiyan Zuo 2 1 Institute of Atmospheric Sciences, Fudan University 2 Chinese Academy of Meteorological
More informationLarge-Scale Circulation Features Typical of Wintertime Extensive and Persistent Low Temperature Events in China
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2011, VOL. 4, NO. 4, 235 241 Large-Scale Circulation Features Typical of Wintertime Extensive and Persistent Low Temperature Events in China BUEH Cholaw 1, 2, FU
More informationOceanic origin of the interannual and interdecadal variability of the summertime western Pacific subtropical high
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L13701, doi:10.1029/2008gl034584, 2008 Oceanic origin of the interannual and interdecadal variability of the summertime western Pacific
More informationInfluence of South China Sea SST and the ENSO on Winter Rainfall over South China CHAN 2,3
Influence of South China Sea SST and the ENSO on Winter Rainfall over South China ZHOU Lian-Tong ( 周连童 ) *1,2, Chi-Yung TAM 2,3, Wen ZHOU( 周文 ) 2,3, and Johnny C. L. CHAN 2,3 1 Center for Monsoon System
More informationThe Formation of Precipitation Anomaly Patterns during the Developing and Decaying Phases of ENSO
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2010, VOL. 3, NO. 1, 25 30 The Formation of Precipitation Anomaly Patterns during the Developing and Decaying Phases of ENSO HU Kai-Ming and HUANG Gang State Key
More informationIntroduction of climate monitoring and analysis products for one-month forecast
Introduction of climate monitoring and analysis products for one-month forecast TCC Training Seminar on One-month Forecast on 13 November 2018 10:30 11:00 1 Typical flow of making one-month forecast Observed
More informationA summer teleconnection pattern over the extratropical Northern Hemisphere and associated mechanisms
Clim Dyn (2010) 35:523 534 DOI 10.1007/s00382-009-0699-0 A summer teleconnection pattern over the extratropical Northern Hemisphere and associated mechanisms Ping Zhao Zuohao Cao Junming Chen Received:
More informationEvaluation of the Twentieth Century Reanalysis Dataset in Describing East Asian Winter Monsoon Variability
ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 30, NO. 6, 2013, 1645 1652 Evaluation of the Twentieth Century Reanalysis Dataset in Describing East Asian Winter Monsoon Variability ZHANG Ziyin 1,2 ( ), GUO Wenli
More information7.6 THE INFLUENCE OF LOW FREQUENCY AND SYNOPTIC VARIABILITY ON THE TIMING, MAGNITUDE, AND GEOGRAPHICAL DISTRIBUTION OF EXTREME WIND EVENTS
7.6 THE INFLUENCE OF LOW FREQUENCY AND SYNOPTIC VARIABILITY ON THE TIMING, MAGNITUDE, AND GEOGRAPHICAL DISTRIBUTION OF EXTREME WIND EVENTS Jeffrey H. Yin* and Grant W. Branstator National Center for Atmospheric
More informationThe Coupled Model Predictability of the Western North Pacific Summer Monsoon with Different Leading Times
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2012, VOL. 5, NO. 3, 219 224 The Coupled Model Predictability of the Western North Pacific Summer Monsoon with Different Leading Times LU Ri-Yu 1, LI Chao-Fan 1,
More informationKUALA LUMPUR MONSOON ACTIVITY CENT
T KUALA LUMPUR MONSOON ACTIVITY CENT 2 ALAYSIAN METEOROLOGICAL http://www.met.gov.my DEPARTMENT MINISTRY OF SCIENCE. TECHNOLOGY AND INNOVATIO Introduction Atmospheric and oceanic conditions over the tropical
More informationLarge-scale atmospheric singularities and summer long-cycle droughts-floods abrupt alternation in the middle and lower reaches of the Yangtze River
Chinese Science Bulletin 2006 Vol. 51 No. 16 2027 2034 DOI: 10.1007/s11434-006-2060-x Large-scale atmospheric singularities and summer long-cycle droughts-floods abrupt alternation in the middle and lower
More informationContrasting impacts of spring thermal conditions over Tibetan Plateau on late-spring to early-summer precipitation in southeast China
ATMOSPHERIC SCIENCE LETTERS Atmos. Sci. Let. 12: 309 315 (2011) Published online 6 May 2011 in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/asl.343 Contrasting impacts of spring thermal conditions
More informationIntroduction of products for Climate System Monitoring
Introduction of products for Climate System Monitoring 1 Typical flow of making one month forecast Textbook P.66 Observed data Atmospheric and Oceanic conditions Analysis Numerical model Ensemble forecast
More informationInterdecadal variability in the thermal difference between western and eastern China and its association with rainfall anomalies
ATMOSPHERIC SCIENCE LETTERS Atmos. Sci. Let. 17: 346 352 (2016) Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/asl.664 Interdecadal variability in the thermal difference
More informationENSO, AO, and climate in Japan. 15 November 2016 Yoshinori Oikawa, Tokyo Climate Center, Japan Meteorological Agency
ENSO, AO, and climate in Japan 15 November 2016 Yoshinori Oikawa, Tokyo Climate Center, Japan Meteorological Agency Aims of this lecture At the end of the yesterday s lecture, Hare-run said, - In the exercise
More informationThe ENSO s Effect on Eastern China Rainfall in the Following Early Summer
ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 26, NO. 2, 2009, 333 342 The ENSO s Effect on Eastern China Rainfall in the Following Early Summer LIN Zhongda ( ) andluriyu( F ) Center for Monsoon System Research,
More informationEast-west SST contrast over the tropical oceans and the post El Niño western North Pacific summer monsoon
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L15706, doi:10.1029/2005gl023010, 2005 East-west SST contrast over the tropical oceans and the post El Niño western North Pacific summer monsoon Toru Terao Faculty
More informationSpring Heavy Rain Events in Taiwan during Warm Episodes and the Associated Large-Scale Conditions
VOLUME 131 MONTHLY WEATHER REVIEW JULY 2003 Spring Heavy Rain Events in Taiwan during Warm Episodes and the Associated Large-Scale Conditions GEORGE TAI-JEN CHEN, ZHIHONG JIANG,* AND MING-CHIN WU Department
More informationPossible Roles of Atlantic Circulations on the Weakening Indian Monsoon Rainfall ENSO Relationship
2376 JOURNAL OF CLIMATE Possible Roles of Atlantic Circulations on the Weakening Indian Monsoon Rainfall ENSO Relationship C.-P. CHANG, PATRICK HARR, AND JIANHUA JU Department of Meteorology, Naval Postgraduate
More informationThe Role of Warm North Atlantic SST in the Formation of Positive Height Anomalies over the Ural Mountains during January 2008
ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 28, NO. 2, 2011, 246 256 The Role of Warm North Atlantic SST in the Formation of Positive Height Anomalies over the Ural Mountains during January 2008 HAN Zhe 1,3
More informationInterannual variations of early summer monsoon rainfall over South China under different PDO backgrounds
INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 31: 847 862 (2011) Published online 25 March 2010 in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/joc.2129 Interannual variations of
More informationThe North Atlantic Oscillation: Climatic Significance and Environmental Impact
1 The North Atlantic Oscillation: Climatic Significance and Environmental Impact James W. Hurrell National Center for Atmospheric Research Climate and Global Dynamics Division, Climate Analysis Section
More informationChapter 1 Climate in 2016
Chapter 1 Climate in 2016 1.1 Global climate summary Extremely high temperatures were frequently observed in many regions of the world, and in particular continued for most of the year in various places
More informationDecrease of light rain events in summer associated with a warming environment in China during
GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L11705, doi:10.1029/2007gl029631, 2007 Decrease of light rain events in summer associated with a warming environment in China during 1961 2005 Weihong Qian, 1 Jiaolan
More informationThe East Asian winter monsoon: Re-amplification in the mid-2000s. WANG Lin* & CHEN Wen
The East Asian winter monsoon: Re-amplification in the mid-2000s WANG Lin* & CHEN Wen Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190,
More informationDistinct linkage between winter Tibetan Plateau snow depth and early summer Philippine Sea anomalous anticyclone
ATMOSPHERIC SCIENCE LETTERS Atmos. Sci. Let. 7: 223 229 (26) Published online 8 February 26 in Wiley Online Library (wileyonlinelibrary.com) DOI:.2/asl.646 Distinct linkage between winter Tibetan Plateau
More informationRainfall variability over the Indochina peninsula during the Boreal Winter, Part I: Preliminary data analysis
Rainfall variability over the Indochina peninsula during the Boreal Winter, Part I: Preliminary data analysis Sirapong Sooktawee*, sirapong@deqp.go.th; Atsamon Limsakul, atsamon@deqp.go.th, Environmental
More informationEurasian Snow Cover Variability and Links with Stratosphere-Troposphere Coupling and Their Potential Use in Seasonal to Decadal Climate Predictions
US National Oceanic and Atmospheric Administration Climate Test Bed Joint Seminar Series NCEP, Camp Springs, Maryland, 22 June 2011 Eurasian Snow Cover Variability and Links with Stratosphere-Troposphere
More informationAnalysis on the decadal scale variation of the dust storm in North China
2260 Science in China Ser. D Earth Sciences 2005 Vol.48 No.12 2260 2266 Analysis on the decadal scale variation of the dust storm in North China KANG Dujuan 1,2 & WANG Huijun 1 1. NZC/LASG, Institute of
More informationWind: Global Systems Chapter 10
Wind: Global Systems Chapter 10 General Circulation of the Atmosphere General circulation of the atmosphere describes average wind patterns and is useful for understanding climate Over the earth, incoming
More informationRecent weakening of northern East Asian summer monsoon: A possible response to global warming
GEOPHYSICAL RESEARCH LETTERS, VOL. 39,, doi:10.1029/2012gl051155, 2012 Recent weakening of northern East Asian summer monsoon: A possible response to global warming Congwen Zhu, 1 Bin Wang, 2 Weihong Qian,
More informationP2.11 DOES THE ANTARCTIC OSCILLATION MODULATE TROPICAL CYCLONE ACTIVITY IN THE NORTHWESTERN PACIFIC
P2.11 DOES THE ANTARCTIC OSCILLATION MODULATE TROPICAL CYCLONE ACTIVITY IN THE NORTHWESTERN PACIFIC Joo-Hong Kim*, Chang-Hoi Ho School of Earth and Environmental Sciences, Seoul National University, Korea
More informationInterdecadal Variations of the East Asian Winter Monsoon and Their Association with Quasi-Stationary Planetary Wave Activity
4860 J O U R N A L O F C L I M A T E VOLUME 22 Interdecadal Variations of the East Asian Winter Monsoon and Their Association with Quasi-Stationary Planetary Wave Activity LIN WANG, RONGHUI HUANG, LEI
More informationThe Planetary Circulation System
12 The Planetary Circulation System Learning Goals After studying this chapter, students should be able to: 1. describe and account for the global patterns of pressure, wind patterns and ocean currents
More informationJournalofGeophysicalResearch: Atmospheres
JournalofGeophysicalResearch: Atmospheres RESEARCH ARTICLE Key Points: There is a connection between the tropical Pacific and the winter climate The SVD2 influence the winter climate over a large area
More informationMonsoon Disturbances Over Southeast and East Asia and the Adjacent Seas
Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas C.-P. Chang Department of Meteorology Naval Postgraduate School, Code MR/Cp Monterey, CA 93943 Telephone 831-656-2840, e-mail cpchang@nps.navy.mil
More informationInstability of the East Asian Summer Monsoon-ENSO Relationship in a coupled global atmosphere-ocean GCM
Instability of the East Asian Summer Monsoon-ENSO Relationship in a coupled global atmosphere-ocean GCM JIANG Dabang 1 WANG Huijun 1 DRANGE Helge 2 LANG Xianmei 1 1 State Key Laboratory of Numerical Modeling
More informationEVALUATION OF BROAD SCALE VERTICAL CIRCULATION AND THERMAL INDICES IN RELATION TO THE ONSET OF INDIAN SUMMER MONSOON
INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 22: 649 661 (2002) Published online in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/joc.742 EVALUATION OF BROAD SCALE VERTICAL CIRCULATION
More informationVerification of the Seasonal Forecast for the 2005/06 Winter
Verification of the Seasonal Forecast for the 2005/06 Winter Shingo Yamada Tokyo Climate Center Japan Meteorological Agency 2006/11/02 7 th Joint Meeting on EAWM Contents 1. Verification of the Seasonal
More informationSpecial blog on winter 2016/2017 retrospective can be found here -
March 4, 2019 Special blog on winter 2016/2017 retrospective can be found here - http://www.aer.com/winter2017 Special blog on winter 2015/2016 retrospective can be found here - http://www.aer.com/winter2016
More informationENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 23 April 2012
ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 23 April 2012 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index
More informationInterannual Teleconnection between Ural-Siberian Blocking and the East Asian Winter Monsoon
Interannual Teleconnection between Ural-Siberian Blocking and the East Asian Winter Monsoon Hoffman H. N. Cheung 1,2, Wen Zhou 1,2 (hoffmancheung@gmail.com) 1 City University of Hong Kong Shenzhen Institute
More informationClimate Outlook for December 2015 May 2016
The APEC CLIMATE CENTER Climate Outlook for December 2015 May 2016 BUSAN, 25 November 2015 Synthesis of the latest model forecasts for December 2015 to May 2016 (DJFMAM) at the APEC Climate Center (APCC),
More informationDynamical prediction of the East Asian winter monsoon by the NCEP Climate Forecast System
JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES, VOL. 118, 1312 1328, doi:10.1002/jgrd.50193, 2013 Dynamical prediction of the East Asian winter monsoon by the NCEP Climate Forecast System Xingwen Jiang,
More informationLong-term Change in Summer Water Vapor Transport over South China in Recent Decades
Journal of the Meteorological Society of Japan, Vol. 89A, pp. 271--282, 2011. 271 DOI:10.2151/jmsj.2011-A17 Long-term Change in Summer Water Vapor Transport over South China in Recent Decades Xiuzhen LI
More informationA sidelong look at storm tracks
ATMOSPHERIC SCIENCE LETTERS Atmos. Sci. Let. 7: 69 74 (2006) Published online in Wiley InterScience (www.interscience.wiley.com).134 A sidelong look at storm tracks I. N. James* and Ulrike Burkhardt School
More informationIncreased Tibetan Plateau Snow Depth An Indicator of the Connection between Enhanced Winter NAO and Late- Spring Tropospheric Cooling over East Asia
ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 27, NO. 4, 2010, 788 794 Increased Tibetan Plateau Snow Depth An Indicator of the Connection between Enhanced Winter NAO and Late- Spring Tropospheric Cooling over
More informationResearch progress of snow cover and its influence on China climate
34 5 Vol. 34 No. 5 2011 10 Transactions of Atmospheric Sciences Oct. 2011. 2011. J. 34 5 627-636. Li Dong-liang Wang Chun-xue. 2011. Research progress of snow cover and its influence on China climate J.
More informationWhy do dust storms decrease in northern China concurrently with the recent global warming?
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L18702, doi:10.1029/2008gl034886, 2008 Why do dust storms decrease in northern China concurrently with the recent global warming? Congwen
More informationSeasonal Climate Outlook for South Asia (June to September) Issued in May 2014
Ministry of Earth Sciences Earth System Science Organization India Meteorological Department WMO Regional Climate Centre (Demonstration Phase) Pune, India Seasonal Climate Outlook for South Asia (June
More informationLong-term changes in total and extreme precipitation over China and the United States and their links to oceanic atmospheric features
INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 34: 286 302 (2014) Published online 27 April 2013 in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/joc.3685 Long-term changes in total
More informationDiurnal cycle of summer rainfall in Shandong of eastern China
INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. (2013) Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/joc.3718 Diurnal cycle of summer rainfall in Shandong of eastern
More informationChapter outline. Reference 12/13/2016
Chapter 2. observation CC EST 5103 Climate Change Science Rezaul Karim Environmental Science & Technology Jessore University of science & Technology Chapter outline Temperature in the instrumental record
More information7 December 2016 Tokyo Climate Center, Japan Meteorological Agency
Summary of the 2016 Asian Summer Monsoon 7 December 2016 Tokyo Climate Center, Japan Meteorological Agency This report summarizes the characteristics of the surface climate and atmospheric/oceanographic
More informationClimate Outlook for March August 2018
The APEC CLIMATE CENTER Climate Outlook for March August 2018 BUSAN, 26 February 2018 The synthesis of the latest model forecasts for March to August 2018 (MAMJJA) from the APEC Climate Center (APCC),
More informationEast China Summer Rainfall during ENSO Decaying Years Simulated by a Regional Climate Model
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2011, VOL. 4, NO. 2, 91 97 East China Summer Rainfall during ENSO Decaying Years Simulated by a Regional Climate Model ZENG Xian-Feng 1, 2, LI Bo 1, 2, FENG Lei
More informationInterannual Relationship between the Winter Aleutian Low and Rainfall in the Following Summer in South China
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2015, VOL. 8, NO. 5, 271 276 Interannual Relationship between the Winter Aleutian Low and Rainfall in the Following Summer in South China SONG Lin-Ye 1,2 and DUAN
More informationImpact of East Asian winter monsoon on the Pacific storm track
METEOROLOGICAL APPLICATIONS Meteorol. Appl. 21: 873 878 (2014) Published online 2 August 2013 in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/met.1423 Impact of East Asian winter monsoon
More informationCharles Jones ICESS University of California, Santa Barbara CA Outline
The Influence of Tropical Variations on Wintertime Precipitation in California: Pineapple express, Extreme rainfall Events and Long-range Statistical Forecasts Charles Jones ICESS University of California,
More informationSensitivity of summer precipitation to tropical sea surface temperatures over East Asia in the GRIMs GMP
GEOPHYSICAL RESEARCH LETTERS, VOL. 40, 1824 1831, doi:10.1002/grl.50389, 2013 Sensitivity of summer precipitation to tropical sea surface temperatures over East Asia in the GRIMs GMP Eun-Chul Chang, 1
More informationClimate Outlook for October 2017 March 2018
The APEC CLIMATE CENTER Climate Outlook for October 2017 March 2018 BUSAN, 25 September 2017 The synthesis of the latest model forecasts for October 2017 to March 2018 (ONDJFM) from the APEC Climate Center
More informationSkills of yearly prediction of the early-season rainfall over southern China by the NCEP climate forecast system
Theor Appl Climatol DOI 10.1007/s00704-014-1333-6 ORIGINAL PAPER Skills of yearly prediction of the early-season rainfall over southern China by the NCEP climate forecast system Siyu Zhao & Song Yang &
More informationUncertainties in Quantitatively Estimating the Atmospheric Heat Source over the Tibetan Plateau
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2014, VOL. 7, NO. 1, 28 33 Uncertainties in Quantitatively Estimating the Atmospheric Heat Source over the Tibetan Plateau DUAN An-Min 1, 3, WANG Mei-Rong 1, 2,
More informationReprint 675. Variations of Tropical Cyclone Activity in the South China Sea. Y.K. Leung, M.C. Wu & W.L. Chang
Reprint 675 Variations of Tropical Cyclone Activity in the South China Sea Y.K. Leung, M.C. Wu & W.L. Chang ESCAP/WMO Typhoon Committee Annual Review 25 Variations in Tropical Cyclone Activity in the South
More informationThe Atmospheric Circulation
The Atmospheric Circulation Vertical structure of the Atmosphere http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/atmosphere/atmospheric_structure.html The global heat engine [courtesy Kevin Trenberth,
More informationDecadal Change in the Correlation Pattern between the Tibetan Plateau Winter Snow and the East Asian Summer Precipitation during
7622 J O U R N A L O F C L I M A T E VOLUME 26 Decadal Change in the Correlation Pattern between the Tibetan Plateau Winter Snow and the East Asian Summer Precipitation during 1979 2011 DONG SI AND YIHUI
More informationSUPPLEMENTARY INFORMATION
Intensification of Northern Hemisphere Subtropical Highs in a Warming Climate Wenhong Li, Laifang Li, Mingfang Ting, and Yimin Liu 1. Data and Methods The data used in this study consists of the atmospheric
More information1. Introduction. 2. Verification of the 2010 forecasts. Research Brief 2011/ February 2011
Research Brief 2011/01 Verification of Forecasts of Tropical Cyclone Activity over the Western North Pacific and Number of Tropical Cyclones Making Landfall in South China and the Korea and Japan region
More informationDepartment of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan
10A.4 TROPICAL CYCLONE FORMATIONS IN THE SOUTH CHINA SEA CHENG-SHANG LEE 1 AND YUNG-LAN LIN* 1, 2 1 Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan 2 Taipei Aeronautic Meteorological
More informationSEASONAL ENVIRONMENTAL CONDITIONS RELATED TO HURRICANE ACTIVITY IN THE NORTHEAST PACIFIC BASIN
SEASONAL ENVIRONMENTAL CONDITIONS RELATED TO HURRICANE ACTIVITY IN THE NORTHEAST PACIFIC BASIN Jennifer M. Collins Department of Geography and Geosciences Bloomsburg University Bloomsburg, PA 17815 jcollins@bloomu.edu
More informationAir Masses of North America cp and ca air masses Air mass characterized by very cold and dry conditions
Chapter 8: Air Masses, Fronts, and Middle-Latitude Cyclones Air masses Fronts Middle-latitude cyclones Air Masses Air mass an extremely large body of air whose properties of temperature and humidity are
More informationNorth Pacific Climate Overview N. Bond (UW/JISAO), J. Overland (NOAA/PMEL) Contact: Last updated: August 2009
North Pacific Climate Overview N. Bond (UW/JISAO), J. Overland (NOAA/PMEL) Contact: Nicholas.Bond@noaa.gov Last updated: August 2009 Summary. The North Pacific atmosphere-ocean system from fall 2008 through
More informationRoles of Anomalous Tibetan Plateau Warming on the Severe 2008 Winter Storm in Central-Southern China
JUNE 2010 B A O E T A L. 2375 Roles of Anomalous Tibetan Plateau Warming on the Severe 2008 Winter Storm in Central-Southern China QING BAO LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences,
More informationSUPPLEMENTARY INFORMATION
doi:10.1038/nature11576 1. Trend patterns of SST and near-surface air temperature Bucket SST and NMAT have a similar trend pattern particularly in the equatorial Indo- Pacific (Fig. S1), featuring a reduced
More informationLong-Term Trend and Decadal Variability of Persistence of Daily 500-mb Geopotential Height Anomalies during Boreal Winter
OCTOBER 2009 D I N G A N D L I 3519 Long-Term Trend and Decadal Variability of Persistence of Daily 500-mb Geopotential Height Anomalies during Boreal Winter RUIQIANG DING AND JIANPING LI State Key Laboratory
More informationDrought in Late Spring of South China in Recent Decades
1JULY 2006 X I N E T A L. 3197 Drought in Late Spring of South China in Recent Decades XIAOGE XIN State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute
More informationResponse of the summer atmospheric circulation over East Asia to SST variability in the tropical Pacific
INTERNATIONAL JOURNAL OF CLIMATOLOGY Int. J. Climatol. 3: 813 86 (1) Published online 17 April 9 in Wiley InterScience (www.interscience.wiley.com) DOI: 1.1/joc.199 Response of the summer atmospheric circulation
More informationEl Niño Seasonal Weather Impacts from the OLR Event Perspective
Science and Technology Infusion Climate Bulletin NOAA s National Weather Service 41 st NOAA Annual Climate Diagnostics and Prediction Workshop Orono, ME, 3-6 October 2016 2015-16 El Niño Seasonal Weather
More informationWinds and Global Circulation
Winds and Global Circulation Atmospheric Pressure Winds Global Wind and Pressure Patterns Oceans and Ocean Currents El Nino How is Energy Transported to its escape zones? Both atmospheric and ocean transport
More informationInterdecadal and Interannnual Variabilities of the Antarctic Oscillation Simulated by CAM3
ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2014, VOL. 7, NO. 6, 515 520 Interdecadal and Interannnual Variabilities of the Antarctic Oscillation Simulated by CAM3 XUE Feng 1, SUN Dan 2,3, and ZHOU Tian-Jun
More informationThe Decadal Shift of the Summer Climate in the Late 1980s over Eastern China and Its Possible Causes
NO.4 ZHANG Renhe, WU Bingyi, ZHAO Ping et al. 435 The Decadal Shift of the Summer Climate in the Late 1980s over Eastern China and Its Possible Causes ZHANG Renhe ( ), WU Bingyi ( ), ZHAO Ping ( ), and
More informationLecture 5: Atmospheric General Circulation and Climate
Lecture 5: Atmospheric General Circulation and Climate Geostrophic balance Zonal-mean circulation Transients and eddies Meridional energy transport Moist static energy Angular momentum balance Atmosphere
More information!"#$%&'()#*+,-./0123 = = = = = ====1970!"#$%& '()* 1980!"#$%&'()*+,-./01"2 !"#$% ADVANCES IN CLIMATE CHANGE RESEARCH
www.climatechange.cn = = = = = 7 = 6!"#$% 211 11 ADVANCES IN CLIMATE CHANGE RESEARCH Vol. 7 No. 6 November 211!"1673-1719 (211) 6-385-8!"#$%&'()#*+,-./123 N O N=!"# $%&=NMMMUNO=!"#$!%&'()*+=NMMNMN = 1979
More informationTransition of the annual cycle of precipitation from double-peak mode to single-peak mode in South China
Article Atmospheric Science November 2013 Vol.58 No.32: 3994 3999 doi: 10.1007/s11434-013-5905-0 Transition of the annual cycle of precipitation from double-peak mode to single-peak mode in South China
More informationAnticorrelated intensity change of the quasi-biweekly and day oscillations over the South China Sea
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L16702, doi:10.1029/2008gl034449, 2008 Anticorrelated intensity change of the quasi-biweekly and 30 50-day oscillations over the South
More informationWhat a Hurricane Needs to Develop
Weather Weather is the current atmospheric conditions, such as air temperature, wind speed, wind direction, cloud cover, precipitation, relative humidity, air pressure, etc. 8.10B: global patterns of atmospheric
More information1. INTRODUCTION: 2. DATA AND METHODOLOGY:
27th Conference on Hurricanes and Tropical Meteorology, 24-28 April 2006, Monterey, CA 3A.4 SUPERTYPHOON DALE (1996): A REMARKABLE STORM FROM BIRTH THROUGH EXTRATROPICAL TRANSITION TO EXPLOSIVE REINTENSIFICATION
More informationNumerical Prediction of the Heavy Rainfall Vortex Over Eastern Asia Monsoon Region
730 Journal of the Meteorological Society of Japan Vol. 62, No. 5 Numerical Prediction of the Heavy Rainfall Vortex Over Eastern Asia Monsoon Region By Shou-Jun Chen* and Lorenzo Dell'Osso European Centre
More informationImpact of the Atlantic Multidecadal Oscillation on the Asian summer monsoon
GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L24701, doi:10.1029/2006gl027655, 2006 Impact of the Atlantic Multidecadal Oscillation on the Asian summer monsoon Riyu Lu, 1,2 Buwen Dong, 3 and Hui Ding 2,4 Received
More informationSea surface temperature east of Australia: A predictor of tropical cyclone frequency over the western North Pacific?
Article Atmospheric Science January 2011 Vol.56 No.2: 196 201 doi: 10.1007/s11434-010-4157-5 SPECIAL TOPICS: Sea surface temperature east of Australia: A predictor of tropical cyclone frequency over the
More informationHigh initial time sensitivity of medium range forecasting observed for a stratospheric sudden warming
GEOPHYSICAL RESEARCH LETTERS, VOL. 37,, doi:10.1029/2010gl044119, 2010 High initial time sensitivity of medium range forecasting observed for a stratospheric sudden warming Yuhji Kuroda 1 Received 27 May
More information