Moist static energy

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1Errata and Updates for Principles of Planetary Climate Last updated **CURRENT** This document contains errata and updates to the first edition of Principles of Planetary Climate by Raymond T. Pierrehumbert. Items marked

Errata and Updates for Principles of Planetary Climate Last updated **CURRENT** This document contains errata and updates to the first edition of Principles of Planetary Climate by Raymond T. Pierrehumbert. Items marked

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Source URL: geosci.uchicago.edu

Language: English - Date: 2013-06-12 18:49:07
2JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, VOL. 5, 1–13, doi:2013MS000270, 2013 Radiative-convective instability Kerry Emanuel,1 Allison A. Wing,1 and Emmanuel M. Vincent1 Received 16 September 2013; revis

JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, VOL. 5, 1–13, doi:2013MS000270, 2013 Radiative-convective instability Kerry Emanuel,1 Allison A. Wing,1 and Emmanuel M. Vincent1 Received 16 September 2013; revis

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Source URL: www.normalesup.org

Language: English - Date: 2014-02-21 16:01:59
3tex file Click here to download LaTeX File (.tex, .sty, .cls, .bst, .bib): Inoue_Back_MSE_revised_2015_0129.tex Generated using version 3.2 of the official AMS LATEX template 1

tex file Click here to download LaTeX File (.tex, .sty, .cls, .bst, .bib): Inoue_Back_MSE_revised_2015_0129.tex Generated using version 3.2 of the official AMS LATEX template 1

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Source URL: www.aos.wisc.edu

Language: English - Date: 2015-02-03 18:17:20
4

PDF Document

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Source URL: ccr.meteor.wisc.edu

Language: English - Date: 2014-03-24 13:53:22
5

PDF Document

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Source URL: ccr.aos.wisc.edu

Language: English - Date: 2014-03-24 13:53:22
6Supplemental Material for ’Clarifying the amount effect’ by Moore et. al., Large-scale tendencies

Supplemental Material for ’Clarifying the amount effect’ by Moore et. al., Large-scale tendencies

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Source URL: www.atmos.washington.edu

Language: English - Date: 2013-10-10 13:42:27
7Figures for Chapter 1 Fig. 1.1 Heavier (shaded) and lighter fluids separated by amovable partition. The dot represents the center of gravity of the two-fluid system. (b) fluids in motion following the removel of the par

Figures for Chapter 1 Fig. 1.1 Heavier (shaded) and lighter fluids separated by amovable partition. The dot represents the center of gravity of the two-fluid system. (b) fluids in motion following the removel of the par

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Source URL: www.atmos.washington.edu

Language: English - Date: 2010-03-30 12:58:59
81 An overview of the kinetic energy cycle in the atmosphere Atmospheric ‡uid motions may be divided into two broad classes, both of which

1 An overview of the kinetic energy cycle in the atmosphere Atmospheric ‡uid motions may be divided into two broad classes, both of which

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Source URL: www.atmos.washington.edu

Language: English - Date: 2010-03-30 12:58:45
9Microsoft Word - MJOFocusGroup_whitepaper_V2.doc

Microsoft Word - MJOFocusGroup_whitepaper_V2.doc

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Source URL: asr.science.energy.gov

Language: English - Date: 2011-07-11 14:38:11
10Generated using V3.0 of the official AMS LATEX template–journal page layout FOR AUTHOR USE ONLY, NOT FOR SUBMISSION! Nonlinear Dynamics and Regional Variations in the MJO Skeleton Andrew J. Majda Department of Mathema

Generated using V3.0 of the official AMS LATEX template–journal page layout FOR AUTHOR USE ONLY, NOT FOR SUBMISSION! Nonlinear Dynamics and Regional Variations in the MJO Skeleton Andrew J. Majda Department of Mathema

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Source URL: met.nps.edu

Language: English - Date: 2011-10-21 13:43:43