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contributor authorMlynczak, Pamela E.
contributor authorSmith, G. Louis
contributor authorWilber, Anne C.
contributor authorStackhouse, Paul W.
date accessioned2017-06-09T16:39:20Z
date available2017-06-09T16:39:20Z
date copyright2011/06/01
date issued2011
identifier issn1558-8424
identifier otherams-71660.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4213576
description abstracthe annual cycles of upward and downward longwave fluxes at the earth?s surface are investigated by use of the NASA Global Energy and Water Cycle Experiment (GEWEX) Surface Radiation Budget Dataset. Principal component analysis is used to quantify the annual cycles. Because of the immense difference between the heat capacity of land and ocean, the surface of the earth is partitioned into these two categories. Over land, the first principal component describes over 95% of the variance of the annual cycle of the upward and downward longwave fluxes. Over ocean the first term describes more than 87% of these annual cycles. Empirical orthogonal functions show the corresponding geographical distributions of these cycles. Phase-plane diagrams of the annual cycles of upward longwave fluxes as a function of net shortwave flux show the thermal inertia of land and ocean.
publisherAmerican Meteorological Society
titleAnnual Cycle of Surface Longwave Radiation
typeJournal Paper
journal volume50
journal issue6
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/2011JAMC2663.1
journal fristpage1212
journal lastpage1224
treeJournal of Applied Meteorology and Climatology:;2011:;volume( 050 ):;issue: 006
contenttypeFulltext


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