Modeling and estimation of snow depth spatial correlation structure from observations over North America

Estimation of spatial correlations should be an integral part of objective analysis of geophysical variables. However, a statistical assessment of spatial correlations has been absent from studies of objective analysis of snow depth since its debut over 2 decades ago. We show a method for computing...

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Main Authors: Cezar Kongoli, Thomas M. Smith
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2023.1035339/full
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author Cezar Kongoli
Cezar Kongoli
Thomas M. Smith
Thomas M. Smith
author_facet Cezar Kongoli
Cezar Kongoli
Thomas M. Smith
Thomas M. Smith
author_sort Cezar Kongoli
collection DOAJ
description Estimation of spatial correlations should be an integral part of objective analysis of geophysical variables. However, a statistical assessment of spatial correlations has been absent from studies of objective analysis of snow depth since its debut over 2 decades ago. We show a method for computing regional spatial correlations of observed snow depth and the daily snow depth increment and fitting them to correlation functions to estimate the correlation scale parameters. Both horizontal and vertical distance correlations are computed from station observations over a well sampled part of North America. The vertical and horizontal distance correlations are fitted to exponential functions using the least square method to estimate the correlation scale parameters including the amplitude, which represents short distance correlation. Our assessment suggests a large horizontal e-folding correlation scale for both the observed snow depth and the daily increment, with implications for improving predictions in poorly monitored areas with relatively flat topography. Over mountainous terrain, vertical e-folding correlation scale for observed snow depth is much smaller than that for the daily snow depth increment and for the snow depth increment used in operational snow analyses. That means that optimal interpolation-based analysis of the increments may be more accurate than the interpolation of snow depth data.
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spelling doaj.art-65789ba682254b93806df09f1afbc8b72023-01-20T12:23:20ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632023-01-011110.3389/feart.2023.10353391035339Modeling and estimation of snow depth spatial correlation structure from observations over North AmericaCezar Kongoli0Cezar Kongoli1Thomas M. Smith2Thomas M. Smith3Earth System Science Interdisciplinary Center (ESSIC), University of Maryland College Park, College Park, MD, United StatesNational Oceanic and Atmospheric Administration (NOAA), National Environmental Satellite, Data, and Information Service (NESDIS), College Park, MD, United StatesEarth System Science Interdisciplinary Center (ESSIC), University of Maryland College Park, College Park, MD, United StatesNational Oceanic and Atmospheric Administration (NOAA), National Environmental Satellite, Data, and Information Service (NESDIS), College Park, MD, United StatesEstimation of spatial correlations should be an integral part of objective analysis of geophysical variables. However, a statistical assessment of spatial correlations has been absent from studies of objective analysis of snow depth since its debut over 2 decades ago. We show a method for computing regional spatial correlations of observed snow depth and the daily snow depth increment and fitting them to correlation functions to estimate the correlation scale parameters. Both horizontal and vertical distance correlations are computed from station observations over a well sampled part of North America. The vertical and horizontal distance correlations are fitted to exponential functions using the least square method to estimate the correlation scale parameters including the amplitude, which represents short distance correlation. Our assessment suggests a large horizontal e-folding correlation scale for both the observed snow depth and the daily increment, with implications for improving predictions in poorly monitored areas with relatively flat topography. Over mountainous terrain, vertical e-folding correlation scale for observed snow depth is much smaller than that for the daily snow depth increment and for the snow depth increment used in operational snow analyses. That means that optimal interpolation-based analysis of the increments may be more accurate than the interpolation of snow depth data.https://www.frontiersin.org/articles/10.3389/feart.2023.1035339/fullsnow depthdaily snow depth incrementspatial correlatione-folding length scalein situ measurement
spellingShingle Cezar Kongoli
Cezar Kongoli
Thomas M. Smith
Thomas M. Smith
Modeling and estimation of snow depth spatial correlation structure from observations over North America
Frontiers in Earth Science
snow depth
daily snow depth increment
spatial correlation
e-folding length scale
in situ measurement
title Modeling and estimation of snow depth spatial correlation structure from observations over North America
title_full Modeling and estimation of snow depth spatial correlation structure from observations over North America
title_fullStr Modeling and estimation of snow depth spatial correlation structure from observations over North America
title_full_unstemmed Modeling and estimation of snow depth spatial correlation structure from observations over North America
title_short Modeling and estimation of snow depth spatial correlation structure from observations over North America
title_sort modeling and estimation of snow depth spatial correlation structure from observations over north america
topic snow depth
daily snow depth increment
spatial correlation
e-folding length scale
in situ measurement
url https://www.frontiersin.org/articles/10.3389/feart.2023.1035339/full
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AT thomasmsmith modelingandestimationofsnowdepthspatialcorrelationstructurefromobservationsovernorthamerica
AT thomasmsmith modelingandestimationofsnowdepthspatialcorrelationstructurefromobservationsovernorthamerica