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Relative Vorticity at the Pressure Level 850 hPa and SSTA in Southeast Asia Causing Precipitation Anomaly over Thailand

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EN
Abstrakty
EN
Monthly relative vorticity and the relative vorticity anomaly at pressure level 850 hPa are computed to study circulation over Southeast Asia associated with the rainfall over Thailand. Monthly mean rainfall is averaged during the years 1979 to 2013 over Thailand to study the trends of rainfall and to analyze the difference between the SSTA in a dry year (1992) and a wet year (1999), and the precipitation anomaly. Rotation of the relative vorticity over Thailand during the rainy season in 1999 is supported by the westerly wind from the Indian Ocean. Relative vorticity over Thailand in October to December are brought by the wind from the east toward the west of the South China Sea. The positive value of relative vorticity in 1992 is less than in 1999. This is consistent with the precipitation anomalies in 1992 and 1999. Clearly, the rainfall and precipitation anomaly over Thailand in wet year 1992 and dry year 1999 are consistent with the relative vorticity at pressure level 850 hPa. Both years are also associated with the SSTA. It can be concluded that the large amounts of rainfall over Thailand are associated with the positive values of relative vorticity at pressure level 850 hPa and SSTA over Southeast Asia. The daily relative vorticity at pressure level 850 hPa and SSTA over Southeast Asia during Typhoon Linda is analyzed in the research. The positive value of relative vorticity is consistent with circulation during Typhoon Linda which is brought by winds from the South China Sea, and the SSTA is also unusual over the Gulf of Thailand and the Andaman Sea. These are the causes of violent storms in Thailand during Typhoon Linda.
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1--12
Opis fizyczny
Bibliogr. 20 poz., rys.
Twórcy
  • Department of Mathematics, Faculty of Science, King Mongkut’s University of Technology Thonburi (KMUTT), 126 Pracha-Uthit Road, Bang Mod, Thung Khru, Bangkok 10140, Thailand
  • The Petchra Pra Jom Klao Scholarship, King Mongkut’s University of Technology Thonburi (KMUTT), 126 Pracha-Uthit Road, Bang Mod, Thung Khru, Bangkok 10140, Thailand
  • Centre of Excellence in Mathematics (CEM), Faculty of Science at Mahidol University, Phayathai Campus, 272 Rama 6 Road, Ratchathewi, Bangkok 10400, Thailand
autor
  • Department of Mathematics, Faculty of Science, King Mongkut’s University of Technology Thonburi (KMUTT), 126 Pracha-Uthit Road, Bang Mod, Thung Khru, Bangkok 10140, Thailand
  • Theoretical and Computational Science Center (TaCS), Science Laboratory Building, Faculty of Science, King Mongkut’s University of Technology Thonburi (KMUTT), 126 Pracha Uthit Road, Bang Mod, Thung Khru, Bangkok 10140, Thailand
  • Ratchaburi Learning Park, King Mongkut’s University of Technology Thonburi, Rang Bua, Chom Bueng, Ratchaburi 70150, Thailand
Bibliografia
  • 1. Adler R.F., Huffman G.J., Chang A., Ferraro R., Xie P.P., Janowiak J., Rudolf B., Schneider U., Curtis S., Bolvin D., Gruber A., Susskind J., Arkin P. and Nelkin E. 2003. The Version-2 Global Precipitation Climatology Project (GPCP) Monthly Precipitation Analysis (1979-present). J. Hydromet, 4, 1147–1167.
  • 2. Aschariyaphotha N., Wongwises P., Humphries U.W. and Wongwises S. 2011. Study of Storm Surge Due to Typhoon Linda (1997) in the Gulf of Thailand Using a Three Dimensional Ocean Model. Applied Mathematics and Computation, 217, 8640–8654.
  • 3. Bartzokas A., Lolis C.J. and Metaxas D.A. 2003. The 850 hPa Relative Vorticity Centres of Action for Winter Precipitation in the Greek Area. Int. J. Climatol. 23, 813–828.
  • 4. Bell M., Available at: http://iridl.ldeo.columbia.edu/dochelp/QA/Basic/anomalies.html, accessed May 2016.
  • 5. Chen J.M., Chen H.S. and Liu J.S. 2013. Coherent Interdecadal Variability of Tropical Cyclone Rainfall and Seasonal Rainfall in Taiwan during October. J. Climate, 26, 308- 321.
  • 6. Climatological Center, Thai Meteorological Department, Available at: http://www.tmd.go.th/programs%5Cuploads%5CyearlySummary%5CAnnual2011_up.pdf, accessed August 2015.
  • 7. Dillon C.P. and Andrews M.J. 1988. Typhoon Linda (30W) 1997 Annual Tropical Cyclone Report. Joint Typhoon Warning Center (JTWC), U.S. Naval Pacific Meteorology and Oceanography Center West JTWC, Naval Oceanography Portal-Public Facing, Hawaii.
  • 8. Felton C.S., Subrahmanyam B. and Murty V.S.N. 2013. ENSO-Modulated Cyclogenesis over the Bay of Bengal. J. Climate, 26, 9806–9818.
  • 9. Harwood R.S., Available at: http://www.geos.ed.ac.uk/~rharwood/teaching/phys4/dynamics/ch_10.pdf, accessed February 2016.
  • 10. Holton J.R. 2004. Mesoscale Circulations. In: An Introduction to Dynamic Meteorology (4th ed.). Elsevier Academic Press, USA.
  • 11. Kalnay E., Kanamitsu M., Kistler R., Collins W., Deaven D., Gandin L., Iredell M., Saha S., White G., Woollen J., Zhu Y., Chelliah M., Ebisuzaki W., Higgins W., Janowiak J., Mo K.C., Ropelewski C., Wang J., Leetmaa A., Reynolds R., Jenne R. and Joseph D. 1996. The NCEP/NCAR 40-Year Reanalysis Project. Bull. Amer. Meteor. Soc., 77(3), 437–471.
  • 12. Krishnamurthy V. and Kirtman B.P. 2009. Relation between Indian Monsoon Variability and SST. J. Climate, 22, 4437–4458.
  • 13. Kroon L.J.M., Available at: http://www.met.wur.nl/education/atmospract/unit19/Div_vortUK.pdf, accessed February 2016.
  • 14. Reynolds R.W., Smith T.M., Liu C., Chelton D.B., Casey K.S. and Schlax M.G. 2007. Daily High Resolution Blended Analyses for Sea Surface Temperature. J. Climate, 20, 5473–5496.
  • 15. Signell R., The U.S. Geological Survey / Geologic Division / Coastal and Marine Program / Woods Hole Field Center, NOAA/National Geophysical Data Center, Marine Geology and Geophysics Division. (n.d.). Coastline Extractor [Online]. Available: http://www.fr73.de/noaa/coast_panama.html [accessed July 2014].
  • 16. Shukla R.P. 2014. The Dominant Intraseasonal Mode of Intraseasonal South Asian Summer Monsoon. J. Geophys. Res. Atmos., 119, 635–651.
  • 17. The NOAA, Available at: https://data.noaa.gov/dataset/kaplan-extended-sst-v2, accessed December 2015.
  • 18. The NOAA/OAR/ESRL, Available at: http://www.esrl.noaa.gov/psd/, accessed December 2015.
  • 19. Wang B., Bao Q., Hoskins B., Wu G. and Liu Y. 2008. Tibetan Plateau Warming and Precipitation Changes in East Asia. Geophys. Res. Lett., 35, 1–5.
  • 20. Yue X. and Wang H. 2008. The Springtime North Asia Cyclone Activity Index and the Southern Annular Mode. Adv. Atmos. Sci., 25(4), 673–679.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-e826f186-bc85-4a32-8421-9ec74abba33b
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