An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature

The presented work focuses on the investigation of gridded daily minimum (<i>TN</i>) and maximum (<i>TX</i>) temperature probability density functions (PDFs) with the intent of both characterising a region and detecting extreme values. The empirical PDFs estimation procedure...

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Main Author: C. Lussana
Format: Article
Language:English
Published: Copernicus Publications 2013-04-01
Series:Advances in Science and Research
Online Access:http://www.adv-sci-res.net/10/59/2013/asr-10-59-2013.pdf
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spelling doaj-4692149932f945c7983d8fe13a8bd77a2020-11-24T20:49:23ZengCopernicus PublicationsAdvances in Science and Research1992-06281992-06362013-04-0110596410.5194/asr-10-59-2013An empirical method for estimating probability density functions of gridded daily minimum and maximum temperatureC. Lussana0ARPA Lombardia, Milano, ItalyThe presented work focuses on the investigation of gridded daily minimum (<i>TN</i>) and maximum (<i>TX</i>) temperature probability density functions (PDFs) with the intent of both characterising a region and detecting extreme values. The empirical PDFs estimation procedure has been realised using the most recent years of gridded temperature analysis fields available at ARPA Lombardia, in Northern Italy. The spatial interpolation is based on an implementation of Optimal Interpolation using observations from a dense surface network of automated weather stations. An effort has been made to identify both the time period and the spatial areas with a stable data density otherwise the elaboration could be influenced by the unsettled station distribution. The PDF used in this study is based on the Gaussian distribution, nevertheless it is designed to have an asymmetrical (skewed) shape in order to enable distinction between warming and cooling events. Once properly defined the occurrence of extreme events, it is possible to straightforwardly deliver to the users the information on a local-scale in a concise way, such as: <i>TX</i> extremely cold/hot or <i>TN</i> extremely cold/hot.http://www.adv-sci-res.net/10/59/2013/asr-10-59-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Lussana
spellingShingle C. Lussana
An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
Advances in Science and Research
author_facet C. Lussana
author_sort C. Lussana
title An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
title_short An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
title_full An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
title_fullStr An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
title_full_unstemmed An empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
title_sort empirical method for estimating probability density functions of gridded daily minimum and maximum temperature
publisher Copernicus Publications
series Advances in Science and Research
issn 1992-0628
1992-0636
publishDate 2013-04-01
description The presented work focuses on the investigation of gridded daily minimum (<i>TN</i>) and maximum (<i>TX</i>) temperature probability density functions (PDFs) with the intent of both characterising a region and detecting extreme values. The empirical PDFs estimation procedure has been realised using the most recent years of gridded temperature analysis fields available at ARPA Lombardia, in Northern Italy. The spatial interpolation is based on an implementation of Optimal Interpolation using observations from a dense surface network of automated weather stations. An effort has been made to identify both the time period and the spatial areas with a stable data density otherwise the elaboration could be influenced by the unsettled station distribution. The PDF used in this study is based on the Gaussian distribution, nevertheless it is designed to have an asymmetrical (skewed) shape in order to enable distinction between warming and cooling events. Once properly defined the occurrence of extreme events, it is possible to straightforwardly deliver to the users the information on a local-scale in a concise way, such as: <i>TX</i> extremely cold/hot or <i>TN</i> extremely cold/hot.
url http://www.adv-sci-res.net/10/59/2013/asr-10-59-2013.pdf
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