Loading…

Changes in Intense Precipitation over the Central United States

In examining intense precipitation over the central United States, the authors consider only days with precipitation when the daily total is above 12.7 mm and focus only on these days and multiday events constructed from such consecutive precipitation days. Analyses show that over the central United...

Full description

Saved in:
Bibliographic Details
Published in:Journal of hydrometeorology 2012-02, Vol.13 (1), p.47-66
Main Authors: Groisman, Pavel Ya, Knight, Richard W., Karl, Thomas R.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173
cites cdi_FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173
container_end_page 66
container_issue 1
container_start_page 47
container_title Journal of hydrometeorology
container_volume 13
creator Groisman, Pavel Ya
Knight, Richard W.
Karl, Thomas R.
description In examining intense precipitation over the central United States, the authors consider only days with precipitation when the daily total is above 12.7 mm and focus only on these days and multiday events constructed from such consecutive precipitation days. Analyses show that over the central United States, a statistically significant redistribution in the spectra of intense precipitation days/events during the past decades has occurred. Moderately heavy precipitation events (within a 12.7–25.4 mm day−1range) became less frequent compared to days and events with precipitation totals above 25.4 mm. During the past 31 yr (compared to the 1948–78 period), significant increases occurred in the frequency of “very heavy” (the daily rain events above 76.2 mm) and extreme precipitation events (defined as daily and multiday rain events with totals above 154.9 mm or 6 in.), with up to 40% increases in the frequency of days and multiday extreme rain events. Tropical cyclones associated with extreme precipitation do not significantly contribute to the changes reported in this study. With time, the internal precipitation structure (e.g., mean and maximum hourly precipitation rates within each preselected range of daily or multiday event totals) did not noticeably change. Several possible causes of observed changes in intense precipitation over the central United States are discussed and/or tested.
doi_str_mv 10.1175/jhm-d-11-039.1
format article
fullrecord <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_968165371</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>24912749</jstor_id><sourcerecordid>24912749</sourcerecordid><originalsourceid>FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173</originalsourceid><addsrcrecordid>eNo9kEtLw0AUhQdRsFa37oTZuUqdO5lHshKJj1YqClpwN6STG5uQTurMVPDfm1Lp6h643zmLj5BLYBMALW_a1TqpEoCEpfkEjsgIJJeJlgKOD1l-npKzEFrGmMghG5HbYlW6Lwy0cXTmIrqA9M2jbTZNLGPTO9r_oKdxhbRAF33Z0YVrIlb0ffhjOCcnddkFvPi_Y7J4fPgopsn89WlW3M0TK4SISS0lMORcZ0qCLrHCrKorXjGrslqImmu91FaximsmbAqpUjyzIIXFpapBp2Nyvd_d-P57iyGadRMsdl3psN8Gk6sMlEw1DORkT1rfh-CxNhvfrEv_a4CZnSjzPH0x90M0gyizK1ztC22IvT_QfBDEtcjTP_AUZMs</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>968165371</pqid></control><display><type>article</type><title>Changes in Intense Precipitation over the Central United States</title><source>JSTOR Archival Journals</source><creator>Groisman, Pavel Ya ; Knight, Richard W. ; Karl, Thomas R.</creator><creatorcontrib>Groisman, Pavel Ya ; Knight, Richard W. ; Karl, Thomas R.</creatorcontrib><description>In examining intense precipitation over the central United States, the authors consider only days with precipitation when the daily total is above 12.7 mm and focus only on these days and multiday events constructed from such consecutive precipitation days. Analyses show that over the central United States, a statistically significant redistribution in the spectra of intense precipitation days/events during the past decades has occurred. Moderately heavy precipitation events (within a 12.7–25.4 mm day−1range) became less frequent compared to days and events with precipitation totals above 25.4 mm. During the past 31 yr (compared to the 1948–78 period), significant increases occurred in the frequency of “very heavy” (the daily rain events above 76.2 mm) and extreme precipitation events (defined as daily and multiday rain events with totals above 154.9 mm or 6 in.), with up to 40% increases in the frequency of days and multiday extreme rain events. Tropical cyclones associated with extreme precipitation do not significantly contribute to the changes reported in this study. With time, the internal precipitation structure (e.g., mean and maximum hourly precipitation rates within each preselected range of daily or multiday event totals) did not noticeably change. Several possible causes of observed changes in intense precipitation over the central United States are discussed and/or tested.</description><identifier>ISSN: 1525-755X</identifier><identifier>EISSN: 1525-7541</identifier><identifier>DOI: 10.1175/jhm-d-11-039.1</identifier><language>eng</language><publisher>American Meteorological Society</publisher><subject>Climate change ; Climate models ; Climatic zones ; Climatology ; El Nino ; Global climate models ; Land use ; Precipitation ; Rain ; Warm seasons</subject><ispartof>Journal of hydrometeorology, 2012-02, Vol.13 (1), p.47-66</ispartof><rights>2012 American Meteorological Society</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173</citedby><cites>FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/24912749$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/24912749$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,58238,58471</link.rule.ids></links><search><creatorcontrib>Groisman, Pavel Ya</creatorcontrib><creatorcontrib>Knight, Richard W.</creatorcontrib><creatorcontrib>Karl, Thomas R.</creatorcontrib><title>Changes in Intense Precipitation over the Central United States</title><title>Journal of hydrometeorology</title><description>In examining intense precipitation over the central United States, the authors consider only days with precipitation when the daily total is above 12.7 mm and focus only on these days and multiday events constructed from such consecutive precipitation days. Analyses show that over the central United States, a statistically significant redistribution in the spectra of intense precipitation days/events during the past decades has occurred. Moderately heavy precipitation events (within a 12.7–25.4 mm day−1range) became less frequent compared to days and events with precipitation totals above 25.4 mm. During the past 31 yr (compared to the 1948–78 period), significant increases occurred in the frequency of “very heavy” (the daily rain events above 76.2 mm) and extreme precipitation events (defined as daily and multiday rain events with totals above 154.9 mm or 6 in.), with up to 40% increases in the frequency of days and multiday extreme rain events. Tropical cyclones associated with extreme precipitation do not significantly contribute to the changes reported in this study. With time, the internal precipitation structure (e.g., mean and maximum hourly precipitation rates within each preselected range of daily or multiday event totals) did not noticeably change. Several possible causes of observed changes in intense precipitation over the central United States are discussed and/or tested.</description><subject>Climate change</subject><subject>Climate models</subject><subject>Climatic zones</subject><subject>Climatology</subject><subject>El Nino</subject><subject>Global climate models</subject><subject>Land use</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Warm seasons</subject><issn>1525-755X</issn><issn>1525-7541</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNo9kEtLw0AUhQdRsFa37oTZuUqdO5lHshKJj1YqClpwN6STG5uQTurMVPDfm1Lp6h643zmLj5BLYBMALW_a1TqpEoCEpfkEjsgIJJeJlgKOD1l-npKzEFrGmMghG5HbYlW6Lwy0cXTmIrqA9M2jbTZNLGPTO9r_oKdxhbRAF33Z0YVrIlb0ffhjOCcnddkFvPi_Y7J4fPgopsn89WlW3M0TK4SISS0lMORcZ0qCLrHCrKorXjGrslqImmu91FaximsmbAqpUjyzIIXFpapBp2Nyvd_d-P57iyGadRMsdl3psN8Gk6sMlEw1DORkT1rfh-CxNhvfrEv_a4CZnSjzPH0x90M0gyizK1ztC22IvT_QfBDEtcjTP_AUZMs</recordid><startdate>20120201</startdate><enddate>20120201</enddate><creator>Groisman, Pavel Ya</creator><creator>Knight, Richard W.</creator><creator>Karl, Thomas R.</creator><general>American Meteorological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20120201</creationdate><title>Changes in Intense Precipitation over the Central United States</title><author>Groisman, Pavel Ya ; Knight, Richard W. ; Karl, Thomas R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Climate change</topic><topic>Climate models</topic><topic>Climatic zones</topic><topic>Climatology</topic><topic>El Nino</topic><topic>Global climate models</topic><topic>Land use</topic><topic>Precipitation</topic><topic>Rain</topic><topic>Warm seasons</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Groisman, Pavel Ya</creatorcontrib><creatorcontrib>Knight, Richard W.</creatorcontrib><creatorcontrib>Karl, Thomas R.</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of hydrometeorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Groisman, Pavel Ya</au><au>Knight, Richard W.</au><au>Karl, Thomas R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in Intense Precipitation over the Central United States</atitle><jtitle>Journal of hydrometeorology</jtitle><date>2012-02-01</date><risdate>2012</risdate><volume>13</volume><issue>1</issue><spage>47</spage><epage>66</epage><pages>47-66</pages><issn>1525-755X</issn><eissn>1525-7541</eissn><abstract>In examining intense precipitation over the central United States, the authors consider only days with precipitation when the daily total is above 12.7 mm and focus only on these days and multiday events constructed from such consecutive precipitation days. Analyses show that over the central United States, a statistically significant redistribution in the spectra of intense precipitation days/events during the past decades has occurred. Moderately heavy precipitation events (within a 12.7–25.4 mm day−1range) became less frequent compared to days and events with precipitation totals above 25.4 mm. During the past 31 yr (compared to the 1948–78 period), significant increases occurred in the frequency of “very heavy” (the daily rain events above 76.2 mm) and extreme precipitation events (defined as daily and multiday rain events with totals above 154.9 mm or 6 in.), with up to 40% increases in the frequency of days and multiday extreme rain events. Tropical cyclones associated with extreme precipitation do not significantly contribute to the changes reported in this study. With time, the internal precipitation structure (e.g., mean and maximum hourly precipitation rates within each preselected range of daily or multiday event totals) did not noticeably change. Several possible causes of observed changes in intense precipitation over the central United States are discussed and/or tested.</abstract><pub>American Meteorological Society</pub><doi>10.1175/jhm-d-11-039.1</doi><tpages>20</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 1525-755X
ispartof Journal of hydrometeorology, 2012-02, Vol.13 (1), p.47-66
issn 1525-755X
1525-7541
language eng
recordid cdi_proquest_miscellaneous_968165371
source JSTOR Archival Journals
subjects Climate change
Climate models
Climatic zones
Climatology
El Nino
Global climate models
Land use
Precipitation
Rain
Warm seasons
title Changes in Intense Precipitation over the Central United States
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-04T22%3A55%3A34IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Changes%20in%20Intense%20Precipitation%20over%20the%20Central%20United%20States&rft.jtitle=Journal%20of%20hydrometeorology&rft.au=Groisman,%20Pavel%20Ya&rft.date=2012-02-01&rft.volume=13&rft.issue=1&rft.spage=47&rft.epage=66&rft.pages=47-66&rft.issn=1525-755X&rft.eissn=1525-7541&rft_id=info:doi/10.1175/jhm-d-11-039.1&rft_dat=%3Cjstor_proqu%3E24912749%3C/jstor_proqu%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c444t-f5510e22786517aede8dfd2d0c68f44f277b7c60d2704c3136628c154ceb6f173%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=968165371&rft_id=info:pmid/&rft_jstor_id=24912749&rfr_iscdi=true