Mesoscale Meteorology in Mid-Latitudes presents the dynamics of mesoscale meteorological phenomena in a highly accessible, student-friendly manner. The book's clear mathematical treatments are complimented by high-quality photographs and illustrations. Comprehensive coverage of subjects including boundary layer mesoscale phenomena, orographic phenomena and deep convection is brought together with the latest developments in the field to provide an invaluable resource for mesoscale meteorology students.
Mesoscale Meteorology in Mid-Latitudes functions as a comprehensive, easy-to-use undergraduate textbook while also providing a useful reference for graduate students, research scientists and weather industry professionals.
Illustrated in full colour throughout
Covers the latest developments and research in the field
Comprehensive coverage of deep convection and its initiation
Uses real life examples of phenomena taken from broad geographical areas to demonstrate the practical aspects of the science
具體描述
讀後感
Chap. 2 p.19 (2.71) from which it is apparent that anticyclonic (Rt < 0) gradient winds are subgeostrophic (i.e., V < Vg) and cyclonic (Rt > 0) gradient winds are supergeostrophic (i.e., V > Vg) Ref: [https://www.theweatherprediction.com/habyh...
評分Chap. 2 p.19 (2.71) from which it is apparent that anticyclonic (Rt < 0) gradient winds are subgeostrophic (i.e., V < Vg) and cyclonic (Rt > 0) gradient winds are supergeostrophic (i.e., V > Vg) Ref: [https://www.theweatherprediction.com/habyh...
評分Chap. 2 p.19 (2.71) from which it is apparent that anticyclonic (Rt < 0) gradient winds are subgeostrophic (i.e., V < Vg) and cyclonic (Rt > 0) gradient winds are supergeostrophic (i.e., V > Vg) Ref: [https://www.theweatherprediction.com/habyh...
評分Chap. 2 p.19 (2.71) from which it is apparent that anticyclonic (Rt < 0) gradient winds are subgeostrophic (i.e., V < Vg) and cyclonic (Rt > 0) gradient winds are supergeostrophic (i.e., V > Vg) Ref: [https://www.theweatherprediction.com/habyh...
評分Chap. 2 p.19 (2.71) from which it is apparent that anticyclonic (Rt < 0) gradient winds are subgeostrophic (i.e., V < Vg) and cyclonic (Rt > 0) gradient winds are supergeostrophic (i.e., V > Vg) Ref: [https://www.theweatherprediction.com/habyh...
用戶評價
為瞭寫中小尺度作業，隻讀瞭第八章。。。
评分為瞭寫中小尺度作業，隻讀瞭第八章。。。
评分寫得很不錯~~
评分寫得很不錯~~
评分寫得很不錯~~
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