Atmospheric convection

Results: 1298



#Item
1Chapter 6 Convection and the Environment In this final chapter we study the ways in which moist convection interacts with the surrounding atmospheric environment. Much of the material in this chapter is not as well under

Chapter 6 Convection and the Environment In this final chapter we study the ways in which moist convection interacts with the surrounding atmospheric environment. Much of the material in this chapter is not as well under

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Source URL: kestrel.nmt.edu

Language: English - Date: 2013-04-23 11:14:40
    2Sensitivity of the hydrologic cycle to surface flux enhancement by convection Ann Casey Hughes1, David Randall2, Charlotte DeMott2, Andrea Jenney2 1Wofford College, Spartanburg, SC and 2Department of Atmospheric Science,

    Sensitivity of the hydrologic cycle to surface flux enhancement by convection Ann Casey Hughes1, David Randall2, Charlotte DeMott2, Andrea Jenney2 1Wofford College, Spartanburg, SC and 2Department of Atmospheric Science,

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    Source URL: esmei.colostate.edu

    Language: English - Date: 2016-07-27 12:52:49
      3From Clouds to Thunderstorms  Carlos Augusto Morales University of São Paulo  Height (km)

      From Clouds to Thunderstorms Carlos Augusto Morales University of São Paulo Height (km)

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      Source URL: pyata.cptec.inpe.br

      Language: English - Date: 2014-05-23 13:33:52
      4Microsoft Word - CLRC2011.doc

      Microsoft Word - CLRC2011.doc

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      Source URL: sti.usra.edu

      Language: English - Date: 2012-11-07 10:48:43
      5WRF-Chem Simulation of Deep Convective Transport in Different Scale Storms using Lightning Data Assimilation Yunyao Li (University of Maryland) Kenneth Pickering, Mary Barth, Megan Bela, Kristin Cummings, Dale Allen,

      WRF-Chem Simulation of Deep Convective Transport in Different Scale Storms using Lightning Data Assimilation Yunyao Li (University of Maryland) Kenneth Pickering, Mary Barth, Megan Bela, Kristin Cummings, Dale Allen,

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      Source URL: www2.mmm.ucar.edu

      Language: English - Date: 2016-07-01 14:03:08
      6P1.30  A SIMPLE 2-DIMENSIONAL CHAOTIC RAIN GUSH MODEL *  Stanley David Gedzelman

      P1.30 A SIMPLE 2-DIMENSIONAL CHAOTIC RAIN GUSH MODEL * Stanley David Gedzelman

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      Source URL: www.sci.ccny.cuny.edu

      Language: English - Date: 2005-07-05 08:59:51
      7Met-infoSynoptic situation: Cold front. Thermal conditions determined by the variable amount of mid-level clouds.

      Met-infoSynoptic situation: Cold front. Thermal conditions determined by the variable amount of mid-level clouds.

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      Source URL: www.flatlandcup.hu

      Language: English - Date: 2009-07-27 03:12:50
      8THE	BIGGER	PICTURE	 							WHAT	CAUSES	WEATHER	CHANGES	and	LONG-TERM	CLIMATE	PATTERNS													 The	 surface	 of	 the	 Sun	 at	 high-temperature	 (~5,000	 0C)	 emits	 most	 of	 its	 solar	 energy	 at	 short wavelength

      THE BIGGER PICTURE WHAT CAUSES WEATHER CHANGES and LONG-TERM CLIMATE PATTERNS The surface of the Sun at high-temperature (~5,000 0C) emits most of its solar energy at short wavelength

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      Source URL: www.nzclimatescience.org

      Language: English - Date: 2016-07-23 18:13:09
      9Errata 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
      10GENERAL AVIATION NEWS Volume 21, Issue 6  June 2013

      GENERAL AVIATION NEWS Volume 21, Issue 6 June 2013

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      Source URL: www.uaoa.org

      Language: English - Date: 2013-05-31 17:56:11