Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression

The relationship between annual rainfall totals and gauge elevation over Great Britain is re-examined using the recently developed technique of geographically weighted regression (GWR). This enables the spatial drift of regression parameters to be identified, estimated and mapped. It is shown that t...

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Autores principales: Salles, M.A., Canziani, P.O., Compagnucci, R.H.
Formato: Artículo publishedVersion
Publicado: 2001
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08998418_v21_n4_p455_Salles
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_08998418_v21_n4_p455_Salles_oai
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id I28-R145-paper_08998418_v21_n4_p455_Salles_oai
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spelling I28-R145-paper_08998418_v21_n4_p455_Salles_oai2024-08-16 Salles, M.A. Canziani, P.O. Compagnucci, R.H. 2001 The relationship between annual rainfall totals and gauge elevation over Great Britain is re-examined using the recently developed technique of geographically weighted regression (GWR). This enables the spatial drift of regression parameters to be identified, estimated and mapped. It is shown that the rate of increase of precipitation with height, or height coefficient, varies from around 4.5 mm/m in the northwest to almost zero in the southeast. There is a particularly rapid change in this value across the English Midlands. The predicted sea level precipitation varies from 1250 mm to less than 600 mm in much the same way. Copyright © 2001 Royal Meteorological Society. Fil:Salles, M.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Canziani, P.O. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Compagnucci, R.H. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. application/pdf http://hdl.handle.net/20.500.12110/paper_08998418_v21_n4_p455_Salles info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Int. J. Climatol. 2001;21(4):455-466 Altitude Great Britain Modelling Precipitation Regression Precipitation (meteorology) Rain Regression analysis Sea level Spatial variations Climatology altitude rainfall raingauge regression analysis spatial variation United Kingdom Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_08998418_v21_n4_p455_Salles_oai
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-145
collection Repositorio Digital de la Universidad de Buenos Aires (UBA)
topic Altitude
Great Britain
Modelling
Precipitation
Regression
Precipitation (meteorology)
Rain
Regression analysis
Sea level
Spatial variations
Climatology
altitude
rainfall
raingauge
regression analysis
spatial variation
United Kingdom
spellingShingle Altitude
Great Britain
Modelling
Precipitation
Regression
Precipitation (meteorology)
Rain
Regression analysis
Sea level
Spatial variations
Climatology
altitude
rainfall
raingauge
regression analysis
spatial variation
United Kingdom
Salles, M.A.
Canziani, P.O.
Compagnucci, R.H.
Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression
topic_facet Altitude
Great Britain
Modelling
Precipitation
Regression
Precipitation (meteorology)
Rain
Regression analysis
Sea level
Spatial variations
Climatology
altitude
rainfall
raingauge
regression analysis
spatial variation
United Kingdom
description The relationship between annual rainfall totals and gauge elevation over Great Britain is re-examined using the recently developed technique of geographically weighted regression (GWR). This enables the spatial drift of regression parameters to be identified, estimated and mapped. It is shown that the rate of increase of precipitation with height, or height coefficient, varies from around 4.5 mm/m in the northwest to almost zero in the southeast. There is a particularly rapid change in this value across the English Midlands. The predicted sea level precipitation varies from 1250 mm to less than 600 mm in much the same way. Copyright © 2001 Royal Meteorological Society.
format Artículo
Artículo
publishedVersion
author Salles, M.A.
Canziani, P.O.
Compagnucci, R.H.
author_facet Salles, M.A.
Canziani, P.O.
Compagnucci, R.H.
author_sort Salles, M.A.
title Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression
title_short Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression
title_full Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression
title_fullStr Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression
title_full_unstemmed Spatial Variations in the Average Rainfall-Altitude Relationship in Great Britain: An Approach using Geographically Weighted Regression
title_sort spatial variations in the average rainfall-altitude relationship in great britain: an approach using geographically weighted regression
publishDate 2001
url http://hdl.handle.net/20.500.12110/paper_08998418_v21_n4_p455_Salles
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_08998418_v21_n4_p455_Salles_oai
work_keys_str_mv AT sallesma spatialvariationsintheaveragerainfallaltituderelationshipingreatbritainanapproachusinggeographicallyweightedregression
AT canzianipo spatialvariationsintheaveragerainfallaltituderelationshipingreatbritainanapproachusinggeographicallyweightedregression
AT compagnuccirh spatialvariationsintheaveragerainfallaltituderelationshipingreatbritainanapproachusinggeographicallyweightedregression
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