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
具体描述
读后感
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...
评分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...
评分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...
评分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...
评分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...
用户评价
写得很不错~~
评分为了写中小尺度作业，只读了第八章。。。
评分为了写中小尺度作业，只读了第八章。。。
评分为了写中小尺度作业，只读了第八章。。。
评分为了写中小尺度作业，只读了第八章。。。
相关图书
本站所有内容均为互联网搜索引擎提供的公开搜索信息，本站不存储任何数据与内容，任何内容与数据均与本站无关，如有需要请联系相关搜索引擎包括但不限于百度，google,bing,sogou 等
© 2025 book.wenda123.org All Rights Reserved. 图书目录大全 版权所有