TCC News 1 No. 29 Summer 2012

Similar documents
Ryuji Yamada Tokyo Climate Center Japan Meteorological Agency E mail: URL:

Tokyo Climate Center s activities as RCC Tokyo

Tokyo Climate Center Website (TCC website) and its products -For monitoring the world climate and ocean-

TCC Recent Development and Activity

Summary of 2005/2006 La Niña Event

Bugs in JRA-55 snow depth analysis

South Asian Climate Outlook Forum (SASCOF-12)

South Asian Climate Outlook Forum (SASCOF-6)

Project Name: Implementation of Drought Early-Warning System over IRAN (DESIR)

Shuhei Maeda Climate Prediction Division Global Environment and Marine Department Japan Meteorological Agency

The benefits and developments in ensemble wind forecasting

Atmospheric circulation analysis for seasonal forecasting

Recent Developments in Climate Information Services at JMA. Koichi Kurihara Climate Prediction Division, Japan Meteorological Agency

Recent Improvement of Integrated Observation Systems in JMA

Summary of the 2007/2008 La Niña Event 1 Summary of Yellow Sand over Japan in Sea Ice in the Sea of Okhotsk for the 2007/2008 Winter Season 5

Interpretation of Outputs from Numerical Prediction System

Winter Forecast for GPC Tokyo. Shotaro TANAKA Tokyo Climate Center (TCC) Japan Meteorological Agency (JMA)

Verification of the Seasonal Forecast for the 2005/06 Winter

Unseasonable weather conditions in Japan in August 2014

Characteristics of Storm Tracks in JMA s Seasonal Forecast Model

No. 20 Spring El Niño Outlook (April October 2010) 1. Contents. (a) (a) (b) (b) Tokyo Climate Center 1 No. 20 Spring 2010

Introduction. 2. Pilot Project 1. EWE. Users. Development of an early warning system for agriculture. User Interface Platform (UIP)

Developing Operational MME Forecasts for Subseasonal Timescales

Application and verification of ECMWF products 2016

Impact of Eurasian spring snow decrement on East Asian summer precipitation

Benefits of the new-generation Himawari-8 geostationary satellite for the Asia-Pacific region. Toshihiko HASHIDA Japan Meteorological Agency (JMA)

The feature of atmospheric circulation in the extremely warm winter 2006/2007

STATUS OF JAPANESE METEOROLOGICAL SATELLITES AND RECENT ACTIVITIES OF MSC

Climate briefing. Wellington region, May Alex Pezza and Mike Thompson Environmental Science Department

FUTURE PLAN AND RECENT ACTIVITIES FOR THE JAPANESE FOLLOW-ON GEOSTATIONARY METEOROLOGICAL SATELLITE HIMAWARI-8/9

Global Temperature 2007: Warmest over land since 1880

JMA s Seasonal Prediction of South Asian Climate for Summer 2018

South Asian Climate Outlook Forum (SASCOF-8)

Introduction of Seasonal Forecast Guidance. TCC Training Seminar on Seasonal Prediction Products November 2013

Weathernews Looks Back at 2015: A Year of Storms. Powerful Typhoons Occurred with Changing Patterns in El Niño Years

Summary. peninsula. likely over. parts of. Asia has. have now. season. There is. season, s that the. declining. El Niño. affect the. monsoon.

Weather Satellite Data Applications for Monitoring and Warning Hazard at BMKG

Fig Operational climatological regions and locations of stations

Dust Storm: An Extreme Climate Event in China

TCC News 1 No. 48 Spring 2017

1. Introduction. 2. Verification of the 2010 forecasts. Research Brief 2011/ February 2011

Primary Factors Contributing to Japan's Extremely Hot Summer of 2010

EL NIÑO/LA NIÑA UPDATE

State of the Climate in Turkey in 2014

Warm Episode over Indian Sub-continent March 2010 By Richard Grumm National Weather Service State College Contributions by Lance Bosart SUNY Albany

COUNTRY REPORT. Jakarta. July, th National Directorate of Meteorology and Geophysics of Timor-Leste (DNMG)

TCC News 1 No. 32 Spring 2013

7 December 2016 Tokyo Climate Center, Japan Meteorological Agency

Data Assimilation of Satellite Lidar Aerosol Observations

NIWA Outlook: October - December 2015

Ganbat.B, Agro meteorology Section

Introduction of Dynamical Regional Downscaling (DSJRA-55) Using the JRA-55 Reanalysis and Discussion for Possibility of its Practical Use

Application and verification of ECMWF products 2017

Chapter 1 Climate in 2016

JMA Contribution to SWFDDP in RAV. (Submitted by Yuki Honda and Masayuki Kyouda, Japan Meteorological Agency) Summary and purpose of document

Understanding Weather and Climate Risk. Matthew Perry Sharing an Uncertain World Conference The Geological Society, 13 July 2017

2013 ATLANTIC HURRICANE SEASON OUTLOOK. June RMS Cat Response

Current status and plans of JMA operational wind product

Special blog on winter 2016/2017 retrospective can be found here -

DEPARTMENT OF EARTH & CLIMATE SCIENCES Name SAN FRANCISCO STATE UNIVERSITY Nov 29, ERTH 360 Test #2 200 pts

The WMO Integrated Global Observing System (WIGOS), current status and planned regional activities

Application and verification of the ECMWF products Report 2007

EL NIÑO/LA NIÑA UPDATE

KUALA LUMPUR MONSOON ACTIVITY CENT

Application and verification of ECMWF products 2012

New Zealand Climate Update No 226, April 2018 Current climate March 2018

Climate Forecast Applications Network (CFAN)

Impacts of the April 2013 Mean trough over central North America

Effect of snow cover on threshold wind velocity of dust outbreak

The next-generation supercomputer and NWP system of the JMA

International Cooperation in Operational Environmental Satellites: The U.S. Experience

Great Lakes Update. Volume 188: 2012 Annual Summary

Development of JMA storm surge model

MODELLING FROST RISK IN APPLE TREE, IRAN. Mohammad Rahimi

June Current Situation and Outlook

Monthly overview. Rainfall

EL NIÑO/LA NIÑA UPDATE

APPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1

South & South East Asian Region:

Great Lakes Update. Volume 199: 2017 Annual Summary. Background

INDIAN OCEAN STATE February 14, 2018 MJO INDEX

Climate Outlook for October 2017 March 2018

Fleet Numerical Meteorology and Oceanography Center. Current Sub-seasonal to Seasonal Capabilities

ALASKA REGION CLIMATE OUTLOOK BRIEFING. December 22, 2017 Rick Thoman National Weather Service Alaska Region

A summary of the weather year based on data from the Zumwalt weather station

Reversal of Arctic Oscillation pattern and its relation to extreme hot summer in Japan in 2010

What is one-month forecast guidance?

Global Flood Awareness System GloFAS

JEFF JOHNSON S Winter Weather Outlook

ENSO, AO, and climate in Japan. 15 November 2016 Yoshinori Oikawa, Tokyo Climate Center, Japan Meteorological Agency

The North Atlantic Oscillation: Climatic Significance and Environmental Impact

Seasonal Climate Watch January to May 2016

Produced by Canadian Ice Service of. 2 December Seasonal Outlook Gulf of St Lawrence and East Newfoundland Waters Winter

Challenges for Climate Science in the Arctic. Ralf Döscher Rossby Centre, SMHI, Sweden

ONE-YEAR EXPERIMENT IN NUMERICAL PREDICTION OF MONTHLY MEAN TEMPERATURE IN THE ATMOSPHERE-OCEAN-CONTINENT SYSTEM

Monitoring Sand and Dust Storms from Space

Seasonal Climate Watch April to August 2018

Sixth Session of the ASEAN Climate Outlook Forum (ASEANCOF-6)

Pacific Decadal Oscillation ( PDO ):

INDIAN OCEAN STATE February 28, 2018 MJO INDEX

Transcription:

No. 29 Summer 2012 Contents Upgrade of JMA s Supercomputer System Summary of Kosa (Aeolian dust) Events over Japan in 2012 Sea Ice in the Sea of Okhotsk for the 2011/2012 Winter Season BMKG expert visit to TCC Page 1 2 4 5 Upgrade of JMA s Supercomputer System The Japan Meteorological Agency (JMA) began operating the latest generation of its Hitachi supercomputer system on 5 June, 2012, with the aim of improving the meteorological information services the Agency provides. The new system, known as Hitachi SR16000/M1, is about 30 times faster than its Hitachi SR11000 predecessor and has the capacity to make more than 800 trillion floating-point calculations per second. The new system allows JMA to run more sophisticated atmospheric and oceanic models, leading to better accuracy and precision in very short-range to long-range forecasting. Using the upgraded supercomputer, JMA plans to improve the one-month forecast model and the seasonal forecast model in a couple of years. The new Japanese reanalysis, JRA-55, which covers from 1958 to 2012 will be completed in the first half of 2013, and its products will be available for operational and research uses around autumn of 2013. (Kazutoshi Onogi, Climate Prediction Division) Table 1 Comparison of Computer Specification Model Old Hitachi SR11000/K1 Hitachi SR11000/J1 New Hitachi SR16000/M1 Theoretical peak performance 27.5 TFlops* 847 TFlops Main memory capacity 13.1 TBytes 108 TBytes (including control) Magnetic disk capacity 18.6 TBytes 348 TBytes * TFlop: capacity to perform one trillion floating-point calculations per second Left: The new supercomputer system used for JMA's weather and climate forecasting Right: New housing for the supercomputer system located in Tokyo TCC News 1 No. 29 Summer 2012

Summary of Kosa (Aeolian dust) Events over Japan in 2012 Characteristics of Kosa events in 2012 From January to June 2012, the number of days on which meteorological stations in Japan observed Kosa was 11, which was below the 1981 2010 normal of 23.1 (Figure 1, left). The total number of stations observing Kosa over the same period was 90, which was also below the normal of 212.7 (Figure 1, right). The first Kosa observation of the year in Japan was made on 24 March, which was the fifth-latest date since records began in 1967, and no further observations were recorded in the country during that month. From mid-january 2012, the Eurasian Continent (especially in the mid-latitudes) experienced significantly lower-than-normal temperatures due to strong cold-air inflow. As a result, the number of days with snow cover was higher than usual in arid areas such as the Gobi Desert and the Ocher Plateau where Kosa originates. Figure 2 shows a distinct difference in the number of days with snow cover for the area in March 2012 (left) and 2006 (right), when Kosa was observed at many stations in Japan. mid-january 2012, the Eurasian Continent, especially in Figure 1 Monthly number of days when meteorological stations in Japan observed Kosa (left), and the monthly total number of stations observing Kosa (right) from January to June 2012 The red and yellow bars show values for 2012 and the 1981 2010 normals, respectively. Figure 2 Anomaly in the number of days with snow cover in East Asia for March 2012 (left) and March 2006 (right) The red boxes in the figures show arid areas such as the Gobi Desert and the Ocher Plateau where Kosa originates. Significant Kosa event in late April Kosa was observed at many stations in eastern and western Japan from 23 to 25 April, and minimum visibility figures of less than 5 km were recorded at several stations in western Japan (Figure 3). A large dust storm formed around the Ocher Plateau from 18 to 19 April. Massive volumes of dust were blown up into the atmosphere and carried over to Japan by upper-air westerly winds. The results of analysis using infrared split-channel images from the MTSAT-2 satellite show that an area of concentrated dust seen around the lower Chang Jiang River early on the morning of 22 April subsequently moved over to western Japan (Figure 4). Figure 3 Meteorological stations observing Kosa and minimum visibility on 24 April TCC News 2 No. 29 Summer 2012

According to JMA s Kosa prediction model, the mass was expected to move over Japan on and after 23 April (Figure 5). Based on this forecast and surface observation reports from the areas in question, JMA released Kosa event information on 24 April in order to call attention to potential traffic hazards. (Nozomu Ohkawara, Atmospheric Environment Division) Figure 4 Kosa area analysis from MTSAT-2 satellite data at 01 JST on 22 April (16 UTC on 21 April, left) and at 24 JST on 22 April (15 UTC on 22 April, right) The red dashed circles in the figures highlight the concentrated dust area that moved over to Japan. Figure 5 Forecast of surface dust concentration by JMA s Kosa prediction model for the period from 15 JST (06 UTC) on 22 April to 21 JST (12 UTC) on 23 April (initial time: 21 JST (12 UTC) on 21 April) Kosa was expected to reach Japan early on the morning of 23 April. TCC News 3 No. 29 Summer 2012

Sea Ice in the Sea of Okhotsk for the 2011/2012 Winter Season The sea ice extent in the Sea of Okhotsk was near normal for the 2012 sea ice season. The sea ice extent in the Sea of Okhotsk was near normal for the 2012 sea ice season (from December 2011 to May 2012) (Figure 6). It reached its seasonal maximum of 112.26 x 10 4 km 2 (slightly below the normal of 116.92 x 10 4 km 2 ) on 31 March (Figures 6 and 7), exceeding the highest value for the previous season (Figures 6 and 8). Figure 8 shows overall trends for the period from 1971 to 2012. Although the sea ice extent in the Sea of Okhotsk shows large interannual variations, there is a long-term downward trend of 173 [63 282] x 10 4 km 2 per decade (the numbers in square brackets indicate the two-sided 95% confidence interval) in the accumulated sea ice extent, and another long-term downward trend of 5.8 [2.0 9.6] x 10 4 km 2 (equivalent to 3.7% of the area of the Sea of Okhotsk) per decade in the maximum extent. (Ryohei Okada, Office of Marine Prediction) Figure 6 Seasonal variation of sea ice extent at five-day intervals in the Sea of Okhotsk from November 2011 to July 2012 Figure 7 Sea ice situation on 31 March 2012 The white area shows the observed sea ice extent, and the red line indicates the extent of normal coverage (1981 2010). Figure 8 Interannual variations in the maximum sea ice extent (red line) and the accumulated sea ice extent (blue line) in the Sea of Okhotsk from 1971 to 2012 Accumulated sea ice extent: the sum of all five-day sea ice extent values from December to May TCC News 4 No. 29 Summer 2012

BMKG expert visit to TCC One of TCC s main tasks is to assist NMHSs in improving their climate services. In addition to running annual training seminars and arranging expert visits, TCC also receives visitors from NMHSs upon request. Indonesia s Meteorological, Climatological and Geophysical Agency (BMKG) is currently developing its Climate Early Warning System (BMKG CEWS), which is scheduled to enter operation in 2013. In a related development, JMA commenced operational provision of Early Warning Information on Extreme Weather (EWIEW)* in March 2008 with the aim of contributing to meteorological risk management in climate-sensitive sectors in Japan. To support the effective development of BMKG CEWS, four experts from BMKG visited TCC in July 2012. During the visit, the BMKG representatives gave informative presentations on their climate services, including those tailored to agriculture in Indonesia. TCC experts then led discussions on a number of relevant issues such as work procedures for the operational climate warning system in Japan and JMA s Ensemble Prediction System (EPS) for seasonal forecasting. Attendees from both organizations engaged in interesting and fruitful discussions on customized climate services and various other issues. The BMKG experts then had exercises on the application of TCC products including gridded EPS data. TCC hopes the visit will contribute to the efficient and effective development of BMKG s planned Climate Warning System. * Japanese site: http://www.jma.go.jp/jp/soukei/ English site: http://www.jma.go.jp/en/soukei/ The amount of information available on the English site is limited. (Teruko Manabe, Tokyo Climate Center) Presentation by a BMKG expert Presentation by a TCC expert Exercises on the application of TCC products BMKG experts and TCC staff members Any comments or inquiry on this newsletter and/or the TCC website would be much appreciated. Please e-mail to tcc@met.kishou.go.jp. (Editors: Teruko Manabe, Ryuji Yamada and Kenji Yoshida) Tokyo Climate Center (TCC), Climate Prediction Division, JMA Address: 1-3-4 Otemachi, Chiyoda-ku, Tokyo 100-8122, Japan TCC Website: http://ds.data.jma.go.jp/tcc/tcc/index.html TCC News 5 No. 29 Summer 2012