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Second Indicator |
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| LEADER |
00000cam a22000003u 4500 |
| 001 |
in00002201230 |
| 005 |
20200226152957.0 |
| 008 |
061113s1982 vau 000 0 eng d |
| 035 |
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|a (OCoLC)ocn227556467
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| 040 |
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|a DTICE
|b eng
|c DTICE
|d OCLCQ
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| 027 |
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|a NORDA-TN-170
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| 029 |
0 |
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|a DTICE
|b ADA122569
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| 035 |
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|a (OCoLC)227556467
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| 049 |
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|a TXAM
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| 086 |
0 |
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|a D 210.109:170
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| 245 |
0 |
4 |
|a The Structure and Energy Budget of the Heat Low Over the Empty Quarter in Saudi Arabia during May 1979.
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| 260 |
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|a Ft. Belvoir
|b Defense Technical Information Center
|c SEP 1982.
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| 300 |
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|a 47 pages
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| 336 |
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|a text
|b txt
|2 rdacontent
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| 337 |
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|a unmediated
|b n
|2 rdamedia
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| 338 |
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|a volume
|b nc
|2 rdacarrier
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| 506 |
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|a APPROVED FOR PUBLIC RELEASE.
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| 520 |
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|a In this paper we present an analysis of a unique data set over the desert area of Saudi Arabia during the northern summer months. The data set comes from the GARP Monsoon Experiment. The paper addresses the thermodynamic budget over the heat low. We examine the role of the horizontal and vertical advective processes, radiative processes, and the vertical eddy flux convergence in the maintenance of the tropical stratification. Satellite observations show that the desert area experiences a net loss of radiation to outer space, while the thermal stratification remains nearly invariant from one day to the next. This study shows that a crucial element in the maintenance of the stratification is the import of heat into this region in the tropical upper troposphere. This energy supply most likely comes from planetary scale divergent circulations.
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| 650 |
1 |
7 |
|a Thermodynamics.
|2 dtict
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| 650 |
1 |
7 |
|a Systems analysis.
|2 dtict
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| 650 |
1 |
7 |
|a Deserts.
|2 dtict
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| 650 |
1 |
7 |
|a Energy conservation.
|2 dtict
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| 650 |
1 |
7 |
|a Atmospheres.
|2 dtict
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| 650 |
2 |
7 |
|a Radiation.
|2 dtict
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| 650 |
2 |
7 |
|a Layers.
|2 dtict
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| 650 |
2 |
7 |
|a Convergence.
|2 dtict
|
| 650 |
2 |
7 |
|a Losses.
|2 dtict
|
| 650 |
2 |
7 |
|a Budgets.
|2 dtict
|
| 650 |
2 |
7 |
|a Surface temperature.
|2 dtict
|
| 650 |
2 |
7 |
|a Advection.
|2 dtict
|
| 650 |
2 |
7 |
|a Eddy currents.
|2 dtict
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| 650 |
2 |
7 |
|a Saudi arabia.
|2 dtict
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| 650 |
2 |
7 |
|a Low altitude.
|2 dtict
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| 650 |
2 |
7 |
|a Monsoons.
|2 dtict
|
| 650 |
1 |
7 |
|a Electric Power Production and Distribution.
|2 scgdst
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| 650 |
2 |
7 |
|a Thermodynamics.
|2 scgdst
|
| 650 |
2 |
7 |
|a Air Breathing Engines(unconventional)
|2 scgdst
|
| 653 |
2 |
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|a Long wave radiation
|
| 653 |
2 |
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|a PE61153N
|
| 700 |
1 |
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|a Blake, D. W.
|
| 700 |
1 |
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|a Krishnamurti, T. N.
|
| 700 |
1 |
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|a Low-Nam, S. V.
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| 700 |
1 |
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|a Fein, J. S.
|
| 710 |
2 |
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|a NAVAL OCEAN RESEARCH AND DEVELOPMENT ACTIVITY NSTL STATION MS.
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| 945 |
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|a cataloged
|b h
|c 2006/11/13
|e revaughan
|f 9:29:56 am
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| 994 |
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|a C0
|b TXA
|
| 999 |
f |
f |
|s 56e64ee6-af14-3864-aea8-9c20066d9e1f
|i 53a68d56-f729-3d30-aece-f62f055182f6
|t 0
|
| 952 |
f |
f |
|p normal
|a Texas A&M University
|b College Station
|c Sterling C. Evans Library
|d Evans: US Documents (Annex 5th floor)
|t 0
|e D 210.109:170
|h Superintendent of Documents classification
|i unmediated -- volume
|m A14834875191
|
| 998 |
f |
f |
|a D 210.109:170
|t 0
|l Evans: US Documents (Annex 5th floor)
|