Atmospheric Moisture during Monsoon 2002 ARMEX Phase I
|
|
- Louisa French
- 5 years ago
- Views:
Transcription
1 Atmospheric Moisture during Monsoon 2002 ARMEX Phase I Anu Simon, K. Mohankumar, Aype Thomas and C.K. Rajan Department of Atmospheric Sciences Cochin University of Science and Technology Cochin
2 All India Rainfall (mm) for June to September 2002 (Climatology is plotted) Oct There was a long dry spell from end June to beginning of August 30-M ay 06-Jun 13-Jun 20-Jun 27-Jun 04-Jul 11-Jul 18-Jul 25-Jul 01-Aug 08-Aug 15-Aug 22-Aug 29-Aug 05-Sep 12-Sep 19-Sep 26-Sep
3 Evolution Of OLR field NOAA(10 dayaverages) JUNE to AUGUST 2002
4 In the present study The moisture field of NCMRWF analysis of the 2002 monsoon (ARMEX Phase I) at levels 1000, 850, 700, 600 and 500 hpa is studied and compared with the and ERA reanalysis data sets.
5 A comparison is also made with the moisture field of monsoon 1998, during which the break monsoon spells were short, using the available and ERA reanalysis data sets.
6 All India Rainfall (mm) for June to September 1998 (Climatology is plotted)
7 Average Specific Humidity(g/kg) -NCMWRF for Arabian sea box (10-20N,55-75 E) 01 June to 31 August hPa 700hPa 14 ALL INDIA DAILY RAINFALL (mm) -JUNE TO SEPTE May 06-Jun 13-Jun 20-Jun 27-Jun 04-Jul 11-Jul 18-Jul 25-Jul 01-Aug 08-Aug 15-Aug 22-Aug 29-Aug 05-Sep 600hPa 500hPa
8 Average Specific Humidity(g/kg) NCMWRF for Bay Of Bengal (10-20N, E) 01 June to 31 August hPa 700hPa 600hPa 500hPa
9 Average Specific Humidity(g/kg) for Arabian sea (10-20N,55-75 E) 01 June 31 August hPa 700hPa 600hPa 500hPa
10 Specfic Humdity (g/kg) 600hPa Specfic Humdity (g/kg) 500hPa Jun 8-Jun 15-Jun 22-Jun 29-Jun 6-Jul 13-Jul 20-Jul 27-Jul 3-Aug 10-Aug 17-Aug 24-Aug 1-Jun 8-Jun 15-Jun 22-Jun 29-Jun 6-Jul 13-Jul 20-Jul 27-Jul 3-Aug 10-Aug 17-Aug 24-Aug Specfic Humdity (g/kg) 600hPa Specfic Humdity (g/kg) 500hPa Jun 8-Jun 15-Jun 22-Jun 29-Jun 6-Jul 13-Jul 20-Jul 27-Jul 3-Aug 10-Aug 17-Aug 24-Aug 1-Jun 8-Jun 15-Jun 22-Jun 29-Jun 6-Jul 13-Jul 20-Jul 27-Jul 3-Aug 10-Aug 17-Aug 24-Aug
11 Evolution Of OLR field NOAA(10 dayaverages) JUNE to AUGUST 1998
12 10 day average of Specific Humidity July JUL 1000 hpa NCMRWF NCMRW JUL1000 hpa NCMRW JUL 1000 hpa F F NCMRWF
13 10 day average of Specific Humidity July 2002 NCMRWF 1-10 JUL 700 hpa JUL 700 hpa NCMRWF JUL 700 hpa NCMRWF
14 1-10 JUL 500 hpa 10 day average of Specific Humidity July 2002 NCMRWF JUL 500 hpa NCMRWF JUL 500 hpa NCMRWF
15 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 July at 1000hPa NCMWRF
16 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 July at 700hPa NCMWRF
17 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 July at 600hPa NCMWRF
18 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 July at 500hPa NCMWRF
19 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 August at 1000hPa NCMWRF
20 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 August at 700hPa NCMWRF
21 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 August at 600hPa NCMWRF
22 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 2002 August at 500hPa NCMWRF NCMWRF
23 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 July at 1000hPa
24 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 July at 700hPa
25 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 July at 600hPa
26 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 July at 500hPa
27 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 August at 1000hPa
28 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 August at 700hPa
29 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 August at 600hPa
30 Wind in m/s (vectors) and Specific Humidity in g/kg (shaded) for 1998 August at 500hPa
31 INTEGRATED MOISTURE FLUX (Kgm -1 s -1 ) ( ) for July 2002 NCMRWF Integrated Flux = 1 g P t P 0 Vq dp
32 INTEGRATED MOISTURE FLUX (Kgm -1 s -1 ) ( ) for July 1998
33 DAILY MOISTURE TRANSPORT ACROSS 75 E FROM 10 20N (kg/day) NCMRWF hPa hPa
34 DAILY MOISTURE TRANSPORT ACROSS 75 E FROM 10 20N (kg/day) hPa
35 DAILY MOISTURE TRANSPORT ACROSS 75 E FROM 10 20N (kg/day) hPa
36 Conclusions During the dry July of 2002 (long break) Arabian Sea had very low moisture at levels above 700hPa Dry air over Arabian sea above 700hPa in July 2002 appears to have come from both the south Indian ocean across the equator and also from the dry continental areas to the north In August, the Arabian sea was more moist with the relatively dry air from the south Indian ocean spreading to south of the Indian peninsula.
37 The moisture field of Bay of Bengal doesn't show much variation during July unlike that of the Arabian Sea. A comparison with the moisture at 600 and 500 hpa levels of 1998 (year with short breaks) show that moisture at these levels in July was more than that of It also remained high throughout the season with very little variations The vertically integrated moisture ( hPa) during July 2002 was relatively less than that during 1998
38 Moisture transport at hpa across the west coast of India (10-20N) during July 2002 was very low compared to August 2002 and also of July & August In general at all levels 1000hPa to 500hPa / has less/more moisture than NCMWRF
39 Thank You
7 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 informationStudy of Intra Annual and Intra Seasonal Variations of Indian Summer Monsoon during ARMEX Period
Study of Intra Annual and Intra Seasonal Variations of Indian Summer Monsoon during ARMEX Period Bhanu Kumar, O.S.R.U., S.Ramalingeswara Rao and K.Muni Krishna Dept. of Meteorology & Oceanography Andhra
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 informationVertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas
Vertical wind shear in relation to frequency of Monsoon Depressions and Tropical Cyclones of Indian Seas Prince K. Xavier and P.V. Joseph Department of Atmospheric Sciences Cochin University of Science
More informationEvidence for Weakening of Indian Summer Monsoon and SA CORDEX Results from RegCM
Evidence for Weakening of Indian Summer Monsoon and SA CORDEX Results from RegCM S K Dash Centre for Atmospheric Sciences Indian Institute of Technology Delhi Based on a paper entitled Projected Seasonal
More informationINFLUENCE OF LARGE-SCALE ATMOSPHERIC MOISTURE FLUXES ON THE INTERANNUAL TO MULTIDECADAL RAINFALL VARIABILITY OF THE WEST AFRICAN MONSOON
3C.4 INFLUENCE OF LARGE-SCALE ATMOSPHERIC MOISTURE FLUXES ON THE INTERANNUAL TO MULTIDECADAL RAINFALL VARIABILITY OF THE WEST AFRICAN MONSOON Andreas H. Fink*, and Sonja Eikenberg University of Cologne,
More informationThe Australian Summer Monsoon
The Australian Summer Monsoon Aurel Moise, Josephine Brown, Huqiang Zhang, Matt Wheeler and Rob Colman Australian Bureau of Meteorology Presentation to WMO IWM-IV, Singapore, November 2017 Outline Australian
More informationSeasonal Climate Watch July to November 2018
Seasonal Climate Watch July to November 2018 Date issued: Jun 25, 2018 1. Overview The El Niño-Southern Oscillation (ENSO) is now in a neutral phase and is expected to rise towards an El Niño phase through
More informationRole of Low Level Jetstream in Intense Monsoon Rainfall episodes over the West Coast of India
Role of Low Level Jetstream in Intense Monsoon Rainfall episodes over the West Coast of India Dr. P.V. Joseph Professor Emeritus Department of Atmospheric Sciences Cochin University of Science and Technology
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 informationContribution of Monthly and Regional Rainfall to the Strength of Indian Summer Monsoon
VOLUME 144 M O N T H L Y W E A T H E R R E V I E W SEPTEMBER 2016 Contribution of Monthly and Regional Rainfall to the Strength of Indian Summer Monsoon YANGXING ZHENG AND M. M. ALI Center for Ocean Atmospheric
More informationDynamics of summer monsoon active phases and onset over Pakistan
Dynamics of summer monsoon active phases and onset over Pakistan F. S. Syed 1, J. H. Yoo 2, H. Körnich 3, F. Kucharski 2 and M. Latif 1 1) Department of Meteorology, COMSATS Institute of Information Technology,
More informationMoist static energy budget diagnostics for. monsoon research. H. Annamalai
Moist static energy budget diagnostics for monsoon research H. Annamalai JJAS Precipitation and SST Climatology I III II Multiple regional heat sources - EIO and SPCZ still experience high precipitation
More informationInter comparison of wave height observations from buoy and altimeter with numerical prediction
Indian Journal of Geo-Marine Sciences Vol. 43(7), July 2014, pp. 1347-1351 Inter comparison of wave height observations from buoy and altimeter with numerical prediction S. A. Sannasiraj 1*, M. Kalyani
More informationThe Abnormal Indian Summer Monsoon of 2002: JRA25 Reanalysis
The Abnormal Indian Summer Monsoon of 2002: JRA25 Reanalysis D. Rajan 1,2, T. Koike 2, J. Matsumoto 2 1 NCMRWF, Ministry of Earth Sciences, India 2 CEOP Lab, University of Tokyo, Japan Correspondence:
More information2011 Atlantic Hurricane Activity and Outlooks A Climate/ Historical Perspective
2011 Atlantic Hurricane Activity and Outlooks A Climate/ Historical Perspective Gerry Bell NOAA Lead Seasonal Hurricane Forecaster Climate Prediction Center/ NWS Related Publications: Bell and Chelliah
More informationVertical Moist Thermodynamic Structure of the MJO in AIRS Observations: An Update and A Comparison to ECMWF Interim Reanalysis
Vertical Moist Thermodynamic Structure of the MJO in AIRS Observations: An Update and A Comparison to ECMWF Interim Reanalysis Baijun Tian 1 Duane Waliser 1, Eric Fetzer 1, and Yuk Yung 2 1.Jet Propulsion
More informationNOTES AND CORRESPONDENCE. Applying the Betts Miller Janjic Scheme of Convection in Prediction of the Indian Monsoon
JUNE 2000 NOTES AND CORRESPONDENCE 349 NOTES AND CORRESPONDENCE Applying the Betts Miller Janjic Scheme of Convection in Prediction of the Indian Monsoon S. S. VAIDYA AND S. S. SINGH Indian Institute of
More informationProbabilistic predictions of monsoon rainfall with the ECMWF Monthly and Seasonal Forecast Systems
Probabilistic predictions of monsoon rainfall with the ECMWF Monthly and Seasonal Forecast Systems Franco Molteni, Frederic Vitart, Tim Stockdale, Laura Ferranti, Magdalena Balmaseda European Centre for
More informationShort-term modulation of Indian summer monsoon rainfall bywest Asian dust
SUPPLEMENTARY INFORMATION DOI: 10.1038/NGEO2107 Short-term modulation of Indian summer monsoon rainfall bywest Asian dust 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 V Vinoj 1,2, Philip J Rasch 1*, Hailong
More informationKalimantan realistically (Figs. 8.23a-d). Also, the wind speeds of the westerly
suppressed rainfall rate (maximum vertical velocity) around 17 LST (Figs. 8.21a-b). These results are in agreement with previous studies (e. g., Emanuel and Raymond 1994). The diurnal variation of maximum
More informationJMA s Seasonal Prediction of South Asian Climate for Summer 2018
JMA s Seasonal Prediction of South Asian Climate for Summer 2018 Atsushi Minami Tokyo Climate Center (TCC) Japan Meteorological Agency (JMA) Contents Outline of JMA s Seasonal Ensemble Prediction System
More informationBMKG Research on Air sea interaction modeling for YMC
BMKG Research on Air sea interaction modeling for YMC Prof. Edvin Aldrian Director for Research and Development - BMKG First Scientific and Planning Workshop on Year of Maritime Continent, Singapore 27-3
More informationGAMINGRE 8/1/ of 7
FYE 09/30/92 JULY 92 0.00 254,550.00 0.00 0 0 0 0 0 0 0 0 0 254,550.00 0.00 0.00 0.00 0.00 254,550.00 AUG 10,616,710.31 5,299.95 845,656.83 84,565.68 61,084.86 23,480.82 339,734.73 135,893.89 67,946.95
More informationFunding provided by NOAA Sectoral Applications Research Project CLIMATE. Basic Climatology Colorado Climate Center
Funding provided by NOAA Sectoral Applications Research Project CLIMATE Basic Climatology Colorado Climate Center Remember These? Factor 1: Our Energy Source Factor 2: Revolution & Tilt Factor 3: Rotation!
More informationLong Range Forecasts of 2015 SW and NE Monsoons and its Verification D. S. Pai Climate Division, IMD, Pune
Long Range Forecasts of 2015 SW and NE Monsoons and its Verification D. S. Pai Climate Division, IMD, Pune Other Contributors: Soma Sen Roy, O. P. Sreejith, Kailas, Madhuri, Pallavi, Mahendra and Jasmine
More informationThe Coupled Earth Reanalysis system [CERA]
The Coupled Earth Reanalysis system [CERA] Patrick Laloyaux Acknowledgments: Eric de Boisséson, Magdalena Balmaseda, Dick Dee, Peter Janssen, Kristian Mogensen, Jean-Noël Thépaut and Reanalysis Section
More informationWhat a Hurricane Needs to Develop
Massive Storms! Hurricanes What a Hurricane Needs to Develop Warm tropical water - at least 80 F High Humidity Light wind Low Pressure Area Form between 5 and 20 latitude Hurricane Ingredients Hurricane
More informationThe spatio-temporal characteristics of total rainfall during September in South Korea according to the variation of ENSO
Clim Dyn DOI 1.17/s382-13-233- The spatio-temporal characteristics of total rainfall during September in South Korea according to the variation of ENSO Ki-Seon Choi Sung-Dae Kang Hae-Dong Kim Bin Wang
More informationClimate of the Philippines and the sea surface temperature effect on summer monsoon rainfall in the Philippines
International Workshop on Climate Downscaling Studies at Tsukuba, October 4, 2017 Climate of the Philippines and the sea surface temperature effect on summer monsoon rainfall in the Philippines Jun Matsumoto
More informationTheoretical and Modeling Issues Related to ISO/MJO
Theoretical and Modeling Issues Related to ISO/MJO Tim Li Department of Meteorology and IPRC University of Hawaii DYNAMO workshop, April 13-14, Boulder, Colorado 1. MJO Initiation issue: Role of air- sea
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 informationNew Salinity Product in the Tropical Indian Ocean Estimated from OLR
New Salinity Product in the Tropical Indian Ocean Estimated from OLR Aquarius Bulusu Subrahmanyam and James J. O Brien Center for Ocean-Atmospheric Prediction Studies, Florida State University V.S.N. Murty
More informationPYROGEOGRAPHY OF THE IBERIAN PENINSULA
PYROGEOGRAPHY OF THE IBERIAN PENINSULA Teresa J. Calado (1), Carlos C. DaCamara (1), Sílvia A. Nunes (1), Sofia L. Ermida (1) and Isabel F. Trigo (1,2) (1) Instituto Dom Luiz, Universidade de Lisboa, Lisboa,
More informationENSO Outlook by JMA. Hiroyuki Sugimoto. El Niño Monitoring and Prediction Group Climate Prediction Division Japan Meteorological Agency
ENSO Outlook by JMA Hiroyuki Sugimoto El Niño Monitoring and Prediction Group Climate Prediction Division Outline 1. ENSO impacts on the climate 2. Current Conditions 3. Prediction by JMA/MRI-CGCM 4. Summary
More informationTime-Space Characteristics of Seasonal and Interannual Variations of Atmospheric Water Balance over South Asia
Journal of the Meteorological Society of Japan, Vol. 87, No. 2, pp. 263--287, 2009. 263 DOI:10.2151/jmsj.87.263 Time-Space Characteristics of Seasonal and Interannual Variations of Atmospheric Water Balance
More informationThe Maritime Continent as a Prediction Barrier
The Maritime Continent as a Prediction Barrier for the MJO Augustin Vintzileos EMC/NCEP SAIC Points to take back home. Forecast of the MJO is at, average, skillful for lead times of up to circa 2 weeks.
More informationThe 2009 Hurricane Season Overview
The 2009 Hurricane Season Overview Jae-Kyung Schemm Gerry Bell Climate Prediction Center NOAA/ NWS/ NCEP 1 Overview outline 1. Current status for the Atlantic, Eastern Pacific and Western Pacific basins
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 informationAverage temperature ( F) World Climate Zones. very cold all year with permanent ice and snow. very cold winters, cold summers, and little rain or snow
P r e v i e w Look carefully at the climagraph of Mumbai, India. What is the wettest month (or months) in Mumbai? What is the driest month (or months) in Mumbai? What effects might this city s climate
More informationStudy of Hydrometeorology in a Hard Rock Terrain, Kadirischist Belt Area, Anantapur District, Andhra Pradesh
Open Journal of Geology, 2012, 2, 294-300 http://dx.doi.org/10.4236/ojg.2012.24028 Published Online October 2012 (http://www.scirp.org/journal/ojg) Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist
More informationWarm Episode over Indian Sub-continent March 2010 By Richard Grumm National Weather Service State College Contributions by Lance Bosart SUNY Albany
Warm Episode over Indian Sub-continent March 2010 By Richard Grumm National Weather Service State College Contributions by Lance Bosart SUNY Albany 1. INTRODUCTION A massive subtropical ridge formed over
More informationPrimary Factors Contributing to Japan's Extremely Hot Summer of 2010
temperature anomalies by its standard deviation for JJA 2010 Primary Factors Contributing to Japan's Extremely Hot Summer of 2010 Nobuyuki Kayaba Climate Prediction Division,Japan Meteorological Agancy
More informationAdvanced Hydrology. (Web course)
Advanced Hydrology (Web course) Subhankar Karmakar Assistant Professor Centre for Environmental Science and Engineering (CESE) Indian Institute of Technology Bombay Powai, Mumbai 400 076 Email: skarmakar@iitb.ac.in
More informationTowards a new understanding of monsoon depressions
Towards a new understanding of monsoon depressions William Boos Dept. of Geology & Geophysics May 2, 25 with contributions from John Hurley & Naftali Cohen Financial support: What is a monsoon low pressure
More informationOperational Monsoon Monitoring at NCEP
Operational Monsoon Monitoring at NCEP Wassila M. Thiaw Climate Prediction Center National Centers for Environmental Predictions Operational Monsoon Monitoring at NCEP Wassila M. Thiaw Climate Prediction
More informationChapter 4 Inter-Annual and Long-Term Variability
Chapter 4 Inter-Annual and Long-Term Variability 4.1 General Rainfa\\ is the most imllortant weather element for India, a trollica\ country. Agriculture, hydro-electric power, industry and the economy
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 informationSeasonal Climate Watch June to October 2018
Seasonal Climate Watch June to October 2018 Date issued: May 28, 2018 1. Overview The El Niño-Southern Oscillation (ENSO) has now moved into the neutral phase and is expected to rise towards an El Niño
More informationExtreme Weather and Climate Week 2. Presented by Ken Sinclair September 29th 2014
Extreme Weather and Climate Week 2 Presented by Ken Sinclair September 29th 2014 Overview Required - Climate extremes and climate change: The Russian heat wave and other climate extremes of 2010 (Trenberth,
More informationA Study of Teleconnection between the South Asian and East Asian Monsoons: Comparison of Summer Monsoon Precipitation of Nepal and South Korea
Journal of Environmental Science International pissn: 1225-4517 eissn: 2287-3503 23(10); 1719~1729; October 2014 http://dx.doi.org/10.5322/jesi.2014.23.10.1719 ORIGINAL ARTICLE A Study of Teleconnection
More informationAnalysis of meteorological measurements made over three rainy seasons in Sinazongwe District, Zambia.
Analysis of meteorological measurements made over three rainy seasons in Sinazongwe District, Zambia. 1 Hiromitsu Kanno, 2 Hiroyuki Shimono, 3 Takeshi Sakurai, and 4 Taro Yamauchi 1 National Agricultural
More informationPresentation Overview. Southwestern Climate: Past, present and future. Global Energy Balance. What is climate?
Southwestern Climate: Past, present and future Mike Crimmins Climate Science Extension Specialist Dept. of Soil, Water, & Env. Science & Arizona Cooperative Extension The University of Arizona Presentation
More informationChiang Rai Province CC Threat overview AAS1109 Mekong ARCC
Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC This threat overview relies on projections of future climate change in the Mekong Basin for the period 2045-2069 compared to a baseline of 1980-2005.
More informationImpacts of precipitation interpolation on hydrologic modeling in data scarce regions
Impacts of precipitation interpolation on hydrologic modeling in data scarce regions 1, Shamita Kumar, Florian Wilken 1, Peter Fiener 1 and Karl Schneider 1 1 Hydrogeography and Climatology Research Group,
More informationInfluences of PBL Parameterizations on Warm-Season Convection-Permitting Regional Climate Simulations
Influences of PBL Parameterizations on Warm-Season Convection-Permitting Regional Climate Simulations Stan Trier (NCAR/MMM) Andreas Prein (NCAR/ASP) and Changhai Liu (NCAR/RAL) GEWEX Convection-Permitting
More informationCHAPTER 8 NUMERICAL SIMULATIONS OF THE ITCZ OVER THE INDIAN OCEAN AND INDONESIA DURING A NORMAL YEAR AND DURING AN ENSO YEAR
CHAPTER 8 NUMERICAL SIMULATIONS OF THE ITCZ OVER THE INDIAN OCEAN AND INDONESIA DURING A NORMAL YEAR AND DURING AN ENSO YEAR In this chapter, comparisons between the model-produced and analyzed streamlines,
More informationImpact of ATOVS data in a mesoscale assimilationforecast system over the Indian region
Impact of ATOVS data in a mesoscale assimilationforecast system over the Indian region John P. George and Munmun Das Gupta National Centre for Medium Range Weather Forecasting, Department of Science &
More informationSeasonal Persistence and Propagation of Intraseasonal Patterns over the Indian Monsoon Region
Seasonal Persistence and Propagation of Intraseasonal Patterns over the Indian Monsoon Region V. Krishnamurthy and J. Shukla Center for Ocean-Land-Atmosphere Studies Institute of Global Environment and
More informationIncreasing frequency of extremely severe cyclonic storms over the Arabian Sea
SUPPLEMENTARY INFORMATION Letters https://doi.org/10.1038/s41558-017-0008-6 In the format provided by the authors and unedited. Increasing frequency of extremely severe cyclonic storms over the Arabian
More informationUpdate on SCOPE-Nowcasting Pilot Project Real Time Ocean Products Suman Goyal Scientist-E
Update on SCOPE-Nowcasting Pilot Project Real Time Ocean Products Suman Goyal Scientist-E 19-22 Nov 2013 SCOPE-Nowcasting-1 Agenda Item 5 Pilot Projects Overview Users /Clients User requirements Product
More informationThe Arctic Energy Budget
The Arctic Energy Budget The global heat engine [courtesy Kevin Trenberth, NCAR]. Differential solar heating between low and high latitudes gives rise to a circulation of the atmosphere and ocean that
More informationWeather Outlook. 1 July 2016 METEOROLOGICAL RESEARCH GROUP. INDIA HEADQUART ERS G 31 Quest Offices DLF Golf Course Road Gurgaon India
Weather Outlook 1 July 2016 METEOROLOGICAL RESEARCH GROUP INDIA HEADQUART ERS G 31 Quest Offices DLF Golf Course Road Gurgaon 122 002 India NORTH AMERICA 350 Fifth Avenue 59 th Floor, New York City NY
More informationSummary and Conclusions
241 Chapter 10 Summary and Conclusions Kerala is situated in the southern tip of India between 8 15 N and 12 50 N latitude and 74 50 E and 77 30 E longitude. It is popularly known as Gods own country.
More informationBasic mechanism for abrupt monsoon transitions
Basic mechanism for abrupt monsoon transitions Anders Levermann, Jacob Schewe, Vladimir Petoukhov, and Hermann Held Earth System Analysis, Potsdam Institute for Climate Impact Research, Potsdam, Germany,
More informationPhysical Features of Monsoon Asia. 192 Unit 7 Teachers Curriculum Institute 60 N 130 E 140 E 150 E 60 E 50 N 160 E 40 N 30 N 150 E.
50 N 60 E 70 E 80 E 90 E 100 E 60 N 110 E 120 E 130 E 140 E 150 E 50 N 160 E 40 N 40 N 30 N 60 E 30 N 150 E Tropic of Cancer 20 N Tropic of Cancer 20 N 10 N 10 N 0 Equator 0 Equator 10 S 10 S 0 500 1,000
More informationWhere does precipitation water come from?
Chapter II Climate and Meteorology Where does precipitation water come from? Introduction The source of water vapor existing over Mongolia has been considered to consist of evapotranspiration at several
More informationCHAPTER 2 DATA AND METHODS. Errors using inadequate data are much less than those using no data at all. Charles Babbage, circa 1850
CHAPTER 2 DATA AND METHODS Errors using inadequate data are much less than those using no data at all. Charles Babbage, circa 185 2.1 Datasets 2.1.1 OLR The primary data used in this study are the outgoing
More informationUPDATE OF REGIONAL WEATHER AND SMOKE HAZE (May 2017)
UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (May 2017) 1. Review of Regional Weather Conditions in April 2017 1.1 Inter monsoon conditions, characterised by afternoon showers and winds that are generally
More informationMekong River Commission
U Mekong River Commission Regional Flood Management and Mitigation Centre Weekly Flood Situation Report for the Mekong River Basin th Prepared on: Monday, /9, covering the week from P P August to 31 st
More informationSAJJAD SAEED¹, MUHAMMAD MUNIR SHEIKH², SYED FAISAL SAEED³
Simulations of 1992 Flood in River Jhelum using High Resolution Regional Climate Model, PRECIS to Study the Underlying Physical Processes Involved in the Extreme Precipitation Event SAJJAD SAEED¹, MUHAMMAD
More informationThe Indian summer monsoon during peaks in the 11 year sunspot cycle
GEOPHYSICAL RESEARCH LETTERS, VOL. 39,, doi:10.1029/2012gl051977, 2012 The Indian summer monsoon during peaks in the 11 year sunspot cycle Harry van Loon 1,2 and Gerald A. Meehl 1 Received 9 April 2012;
More informationARUBA CLIMATOLOGICAL SUMMARY 2014 PRECIPITATION
ARUBA CLIMATOLOGICAL SUMMARY 2014 PRECIPITATION The total amount of rainfall recorded at Reina Beatrix International Airport for the year 2014 was 309.2 mm. This is 34.4 % below normal ( Figure 1 ). During
More informationModeling Indian Ocean Biogeochemistry Iron Limitation and Dipole-Zonal Mode Impacts
Modeling Indian Ocean Biogeochemistry Iron Limitation and Dipole-Zonal Mode Impacts Jerry Wiggert jwiggert@ccpo.odu.edu Funded by the NASA Oceanography Program Outline 1) Coupled 3-D Bio-physical Model
More informationStudy of Changes in Climate Parameters at Regional Level: Indian Scenarios
Study of Changes in Climate Parameters at Regional Level: Indian Scenarios S K Dash Centre for Atmospheric Sciences Indian Institute of Technology Delhi Climate Change and Animal Populations - The golden
More informationGovernment of Sultanate of Oman Public Authority of Civil Aviation Directorate General of Meteorology. National Report To
Government of Sultanate of Oman Public Authority of Civil Aviation Directorate General of Meteorology National Report To Panel on Tropical Cyclones in the Bay of Bengal And Arabian Sea 43rd Session, India
More informationThe 2014 Atlantic Hurricane Season. What is New and What to Expect. Mark Chambers President & CEO ImpactWeather, Inc.
The 2014 Atlantic Hurricane Season What is New and What to Expect Mark Chambers President & CEO ImpactWeather, Inc. Hurricane Climatology for the Gulf of Mexico A Look back at 2013 The outlook for this
More informationLAB J - WORLD CLIMATE ZONES
Introduction LAB J - WORLD CLIMATE ZONES The objective of this lab is to familiarize the student with the various climates around the world and the climate controls that influence these climates. Students
More informationovember 2008 Antigua and Barbuda Meteorological Service
ovember 2008 Antigua and Barbuda Meteorological Service The Atlantic Hurricane Season Summary 2008 Special Focus on Antigua and Barbuda The Season in Brief Sixteen (16) named storms formed in the Atlantic
More informationARUBA CLIMATOLOGICAL SUMMARY 2017 PRECIPITATION
ARUBA CLIMATOLOGICAL SUMMARY 2017 PRECIPITATION The total amount of rainfall recorded at Reina Beatrix International Airport for the year 2017 was 391.0 mm. This is 17.1 % below normal ( Figure 1 ). During
More informationStephen W. Bieda III, Steven L. Mullen, Christopher L. Castro University of Arizona Department of Atmospheric Sciences
Stephen W. Bieda III, Steven L. Mullen, Christopher L. Castro University of Arizona Department of Atmospheric Sciences Collaborative effort between National Weather Service, Tucson, AZ WSFO and the University
More informationCURRENT STATUS OF MONSOON Main Meteorological conditions of the last week (27August to 2 September)
CURRENT STATUS OF MONSOON 2009 Main Meteorological conditions of the last week (27August to 2 September) Last week s low pressure area over Orissa and neighbourhood moved west-northwestwards across central
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 informationWATER VAPOR FLUXES OVER EQUATORIAL CENTRAL AFRICA
WATER VAPOR FLUXES OVER EQUATORIAL CENTRAL AFRICA INTRODUCTION A good understanding of the causes of climate variability depend, to the large extend, on the precise knowledge of the functioning of the
More informationSeasonal Climate Watch April to August 2018
Seasonal Climate Watch April to August 2018 Date issued: Mar 23, 2018 1. Overview The El Niño-Southern Oscillation (ENSO) is expected to weaken from a moderate La Niña phase to a neutral phase through
More informationUniversity of Reading, Reading, United Kingdom. 2 Hadley Centre for Climate Prediction and Research, Meteorological Office, Exeter, United Kingdom.
9.1 RUNNING A CLIMATE MODEL IN FORECAST MODE TO IDENTIFY THE SOURCE OF TROPICAL CLIMATE ERRORS: WITH SPECIFIC REFERENCE TO THE DRY BIAS OVER THE MARITIME CONTINENT IN AN ATMOSPHERE ONLY GCM 1 Jane Strachan,
More informationAssessing the impact of Arctic sea ice variability on Greenland Ice Sheet surface mass and energy exchange
Assessing the impact of Arctic sea ice variability on Greenland Ice Sheet surface mass and energy exchange J. Stroeve, L. Boisvert, J. Mioduszewski, T. Komayo Enhanced Greenland Melt and Sea Ice Loss R=
More informationWhat is the difference between Weather and Climate?
What is the difference between Weather and Climate? Objective Many people are confused about the difference between weather and climate. This makes understanding the difference between weather forecasts
More informationClimate Variability in South Asia
Climate Variability in South Asia V. Niranjan, M. Dinesh Kumar, and Nitin Bassi Institute for Resource Analysis and Policy Contents Introduction Rainfall variability in South Asia Temporal variability
More informationMassive Storms! 8.10C Identify the role of the oceans in the formation of weather systems such as hurricanes
Massive Storms! 8.10C Identify the role of the oceans in the formation of weather systems such as hurricanes Instructional page: Each person in group will take on one portion or set of questions: Each
More information2016 Meteorology Summary
2016 Meteorology Summary New Jersey Department of Environmental Protection AIR POLLUTION AND METEOROLOGY Meteorology plays an important role in the distribution of pollution throughout the troposphere,
More informationSEA ICE PREDICTION NETWORK (SIPN) Template for Pan-Arctic Sea Ice Outlook Core Contributions August 2015 Report
SEA ICE PREDICTION NETWORK (SIPN) Template for Pan-Arctic Sea Ice Outlook Core Contributions August 2015 Report 1. David Rennie / Amateur Individual 2. Executive summary This estimate is primarily based
More informationIntraseasonal Oscillations and Interannual Variability of the Indian Summer Monsoon
1180 JOURNAL OF CLIMATE Intraseasonal Oscillations and Interannual Variability of the Indian Summer Monsoon B. N. GOSWAMI AND R. S. AJAYA MOHAN Centre for Atmospheric and Oceanic Sciences, Indian Institute
More information3. HYDROMETEROLOGY. 3.1 Introduction. 3.2 Hydro-meteorological Aspect. 3.3 Rain Gauge Stations
3. HYDROMETEROLOGY 3.1 Introduction Hydrometeorology is a branch of meteorology and hydrology that studies the transfer of water and energy between the land surface and the lower atmosphere. Detailed hydrological
More informationCharacteristics of 2014 summer climate over South Korea
2 nd East Asia winter Climate Outlook Forum Characteristics of 2014 summer climate over South Korea October 30, 2014 So-Young Yim, E-hyung Park, and Hyun-Sook Jung Climate Prediction Division Korea Meteorological
More informationSupplementary Figure 1. Summer mesoscale convective systems rainfall climatology and trends. Mesoscale convective system (MCS) (a) mean total
Supplementary Figure 1. Summer mesoscale convective systems rainfall climatology and trends. Mesoscale convective system (MCS) (a) mean total rainfall and (b) total rainfall trend from 1979-2014. Total
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 informationMonday 7 October 2013, Class #15
Monday 7 October 2013, Class #15 Concepts for Today (Basics for Thermodynamics) Weather versus climate Lapse Rate (Adiabatic Lapse Rate) Ideal Gas Law Adiabatic Processes Potential Temperature Hydrostatic
More informationEquatorial Waves and Air Sea Interaction in the Boreal Summer Intraseasonal Oscillation
1JULY 2001 KEMBALL-COOK AND WANG 2923 Equatorial Waves and Air Sea Interaction in the Boreal Summer Intraseasonal Oscillation SUSAN KEMBALL-COOK* AND BIN WANG Department of Meteorology, School of Ocean
More informationWMO technical conference on climate services building on clips legacy
WMO technical conference on climate services building on clips legacy conjunction with the Sixteenth Session of WMO Commission for Climatology (CCl-16) and the 35 th Meeting of the Joint Scientific Committee
More information