Radiosonde

Results: 676



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61APPENDIX A REFERENCES 1. Buck, A.L. New Equations for Computing Vapor Pressure and Enhancement Factor. J. Applied Meteorology, 20, , 1981.

APPENDIX A REFERENCES 1. Buck, A.L. New Equations for Computing Vapor Pressure and Enhancement Factor. J. Applied Meteorology, 20, , 1981.

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Source URL: www.ofcm.noaa.gov

Language: English - Date: 2006-07-31 15:42:32
62National Climatic Data Center DATA DOCUMENTATION FOR DATASETDSIRadiosonde Replacement System - 1 second BUFR

National Climatic Data Center DATA DOCUMENTATION FOR DATASETDSIRadiosonde Replacement System - 1 second BUFR

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Source URL: www1.ncdc.noaa.gov

Language: English - Date: 2008-08-13 10:22:47
63Uncertainty of the Stratospheric/Tropospheric Temperature Trends in: Multiple Reanalyses, MSUs and Radiosondes JIANJUN XU Environmental Science and Technology Center, College of Science, George Mason University

Uncertainty of the Stratospheric/Tropospheric Temperature Trends in: Multiple Reanalyses, MSUs and Radiosondes JIANJUN XU Environmental Science and Technology Center, College of Science, George Mason University

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Source URL: ee.nmt.edu

Language: English - Date: 2012-04-02 10:32:06
64PALAU project by JAMSTEC Pacific Area Long-term Atmospheric observation for Understanding of climate change Tropical Western Pacific is a key area to understand the air-sea interaction and the tropical-extratropical inte

PALAU project by JAMSTEC Pacific Area Long-term Atmospheric observation for Understanding of climate change Tropical Western Pacific is a key area to understand the air-sea interaction and the tropical-extratropical inte

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Source URL: www.jamstec.go.jp

Language: English - Date: 2015-04-15 20:17:37
65APPENDIX F ARCHIVING F.1 Introduction. There are many critical non-real-time users of rawinsonde observations in climatology and research. In order to make rawinsonde observations available to retrospective users, observ

APPENDIX F ARCHIVING F.1 Introduction. There are many critical non-real-time users of rawinsonde observations in climatology and research. In order to make rawinsonde observations available to retrospective users, observ

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Source URL: www.ofcm.noaa.gov

Language: English - Date: 2006-07-31 15:43:11
66Technical Sessions B. E. Manner National Oceanic and Atmospheric Administration Wave Propagation Laboratory 130ulder, CO 80303

Technical Sessions B. E. Manner National Oceanic and Atmospheric Administration Wave Propagation Laboratory 130ulder, CO 80303

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Source URL: www.arm.gov

Language: English - Date: 2009-08-28 12:42:35
67Methods of measuring the speed and direction of the wind in th

Methods of measuring the speed and direction of the wind in th

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Source URL: www.ofcm.noaa.gov

Language: English - Date: 2006-07-31 15:42:21
68APPENDIX G GLOSSARY -AAdiabatic process. A thermodynamic change of state of a system in which there is no transfer of heat or mass across the boundaries of the system. In an adiabatic process, compression always results

APPENDIX G GLOSSARY -AAdiabatic process. A thermodynamic change of state of a system in which there is no transfer of heat or mass across the boundaries of the system. In an adiabatic process, compression always results

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Source URL: www.ofcm.noaa.gov

Language: English - Date: 2006-07-31 15:43:15
69CHAPTER 1 INTRODUCTION 1.1 Purpose and Scope. A radiosonde is a balloon-borne instrument used to simultaneously measure and transmit meteorological data while ascending through the atmosphere. The instrument consists of

CHAPTER 1 INTRODUCTION 1.1 Purpose and Scope. A radiosonde is a balloon-borne instrument used to simultaneously measure and transmit meteorological data while ascending through the atmosphere. The instrument consists of

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Source URL: www.ofcm.noaa.gov

Language: English - Date: 2006-07-31 15:41:41
70NPOESS Remanifestation Cost Study Kick-off

NPOESS Remanifestation Cost Study Kick-off

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Source URL: www1.ncdc.noaa.gov

Language: English - Date: 2010-06-15 14:16:11