Mesoscale Meteorology in Midlatitudes 在线电子书 pdf 下载 txt下载 epub 下载 mobi 下载 2024


Mesoscale Meteorology in Midlatitudes

简体网页||繁体网页
Paul M. Markowski 作者
Wiley
Yvette P. Richardson 译者
2010-3-2 出版日期
430 页数
$69.84 价格
丛书系列
9780470742136 图书编码

Mesoscale Meteorology in Midlatitudes 在线电子书 图书标签: 气象学  美国  科学  大气科学  2014   


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发表于2024-11-23


Mesoscale Meteorology in Midlatitudes 在线电子书 epub 下载 mobi 下载 pdf 下载 txt 下载 2024

Mesoscale Meteorology in Midlatitudes 在线电子书 epub 下载 mobi 下载 pdf 下载 txt 下载 2024

Mesoscale Meteorology in Midlatitudes 在线电子书 pdf 下载 txt下载 epub 下载 mobi 下载 2024



Mesoscale Meteorology in Midlatitudes 在线电子书 用户评价

评分

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

写得很不错~~

评分

写得很不错~~

Mesoscale Meteorology in Midlatitudes 在线电子书 著者简介


Mesoscale Meteorology in Midlatitudes 在线电子书 图书目录


Mesoscale Meteorology in Midlatitudes 在线电子书 pdf 下载 txt下载 epub 下载 mobi 在线电子书下载

Mesoscale Meteorology in Midlatitudes 在线电子书 图书描述

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

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Mesoscale Meteorology in Midlatitudes 在线电子书 读后感

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...

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...

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