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contributor authorJohnson, Gregory L.
contributor authorHanson, Clayton L.
date accessioned2017-06-09T14:09:24Z
date available2017-06-09T14:09:24Z
date copyright1995/01/01
date issued1995
identifier issn0894-8763
identifier otherams-13454.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148906
description abstractUsing rotated principal component analysis (PCA), unique, orthogonal spatial patterns of daily and monthlyprecipitation on a well-instrumented, mountainous watershed in Idaho are examined for their relationship totopography, geographic location, and atmospheric variability. Precipitation pattern and homogeneous precipitationregion differences between daily and monthly timescales and between winter and summer Seasons were identifiedusing the rotated PCA procedure. In general, monthly data produced regional boundaries more closely alignedwith topography, reflecting the integration of many storm events on monthly timescales. Spatial fields, derivedfrom mapping rotated component loadings at 46 precipitation stations on a 234-kmz watershed, were found tobe highly correlated with topography and geographic location. The eight-year time series of the components forspecific watershed regions were found to be moderately related to linear combinations of meteorological variablesderived from a single radiosonde station approximately 50 km from the waterhed. This would indicate thepotential usefulness of data from a single location, such as a general circulation model grid point, to provideclues about spatial pattern changes and regional precipitation fluctuations even on a small watershed, if sufficientinformation about local climate (i.e., topographic influences) is first established.
publisherAmerican Meteorological Society
titleTopographic and Atmospheric Influences on Precipitation Variability over a Mountainous Watershed
typeJournal Paper
journal volume34
journal issue1
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450-34.1.68
journal fristpage68
journal lastpage87
treeJournal of Applied Meteorology:;1995:;volume( 034 ):;issue: 001
contenttypeFulltext


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