On the asymmetric distribution of shear-relative typhoon rainfall
Autor: | Zhifan Chen, Tim Li, Si Gao, Shunan Zhai |
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Rok vydání: | 2017 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Advection 0208 environmental biotechnology 02 engineering and technology Moisture advection 01 natural sciences 020801 environmental engineering Typhoon Climatology Wind shear Subtropical ridge Environmental science Precipitation Tropical cyclone Tropical cyclone rainfall forecasting 0105 earth and related environmental sciences |
Zdroj: | Meteorology and Atmospheric Physics. 130:11-22 |
ISSN: | 1436-5065 0177-7971 |
DOI: | 10.1007/s00703-016-0499-0 |
Popis: | The Tropical Rainfall Measuring Mission (TRMM) 3B42 precipitation, the National Centers for Environmental Prediction (NCEP) Final analysis and the Regional Specialized Meteorological Center (RSMC) Tokyo best-track data during 2000–2015 are used to compare spatial rainfall distribution associated with Northwest Pacific tropical cyclones (TCs) with different vertical wind shear directions and investigate possible mechanisms. Results show that the maximum TC rainfall are all located in the downshear left quadrant regardless of shear direction, and TCs with easterly shear have greater magnitudes of rainfall than those with westerly shear, consistent with previous studies. Rainfall amount of a TC is related to its relative position and proximity from the western Pacific subtropical high (WPSH) and the intensity of water vapor transport, and low-level jet is favorable for water vapor transport. The maximum of vertically integrated moisture flux convergence (MFC) are located on the downshear side regardless of shear direction, and the contribution of wind convergence to the total MFC is far larger than that of moisture advection. The cyclonic displacement of the maximum rainfall relative to the maximum MFC is possibly due to advection of hydrometeors by low- and middle-level cyclonic circulation of TCs. The relationship between TC rainfall and the WPSH through water vapor transport and vertical wind shear implies that TC rainfall may be highly predictable given the high predictability of the WPSH. |
Databáze: | OpenAIRE |
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