The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S
Abstract. North Atlantic sea surface temperatures for 1856-1999 contain a 65-80 year cycle with a 0.4 C range, referred to as the Atlantic Multidecadal Oscillation (AMO) by Kerr [2000]. AMO warm phases occurred during 1860-1880 and 1940-1960, and cool phases during 1905-1925 and 1970-1990. The signa...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.586.6168 2023-05-15T17:29:31+02:00 The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S David B. En Eld Alberto M. Mestas-nu~nez Paul J. Trimble The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.6168 http://www.aoml.noaa.gov/phod/docs/enfield/enfield_etal2001.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.6168 http://www.aoml.noaa.gov/phod/docs/enfield/enfield_etal2001.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aoml.noaa.gov/phod/docs/enfield/enfield_etal2001.pdf text 2001 ftciteseerx 2016-01-08T13:17:42Z Abstract. North Atlantic sea surface temperatures for 1856-1999 contain a 65-80 year cycle with a 0.4 C range, referred to as the Atlantic Multidecadal Oscillation (AMO) by Kerr [2000]. AMO warm phases occurred during 1860-1880 and 1940-1960, and cool phases during 1905-1925 and 1970-1990. The signal is global in scope, with a posi-tively correlated co-oscillation in parts of the North Pa-ci c, but it is most intense in the North Atlantic and cov-ers the entire basin there. During AMO warmings most of the United States sees less than normal rainfall, including Midwest droughts in the 1930s and 1950s. Between AMO warm and cool phases, Mississippi River outflow varies by 10 % while the inflow to Lake Okeechobee, Florida varies by 40%. The geographical pattern of variability is influenced mainly by changes in summer rainfall. The winter patterns of interannual rainfall variability associated with El Ni~no-Southern Oscillation are also signicantly changed between AMO phases. Text North Atlantic Unknown Kerr ENVELOPE(65.633,65.633,-70.433,-70.433) Posi ENVELOPE(24.179,24.179,65.691,65.691) |
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Open Polar |
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Unknown |
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ftciteseerx |
language |
English |
description |
Abstract. North Atlantic sea surface temperatures for 1856-1999 contain a 65-80 year cycle with a 0.4 C range, referred to as the Atlantic Multidecadal Oscillation (AMO) by Kerr [2000]. AMO warm phases occurred during 1860-1880 and 1940-1960, and cool phases during 1905-1925 and 1970-1990. The signal is global in scope, with a posi-tively correlated co-oscillation in parts of the North Pa-ci c, but it is most intense in the North Atlantic and cov-ers the entire basin there. During AMO warmings most of the United States sees less than normal rainfall, including Midwest droughts in the 1930s and 1950s. Between AMO warm and cool phases, Mississippi River outflow varies by 10 % while the inflow to Lake Okeechobee, Florida varies by 40%. The geographical pattern of variability is influenced mainly by changes in summer rainfall. The winter patterns of interannual rainfall variability associated with El Ni~no-Southern Oscillation are also signicantly changed between AMO phases. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
David B. En Eld Alberto M. Mestas-nu~nez Paul J. Trimble |
spellingShingle |
David B. En Eld Alberto M. Mestas-nu~nez Paul J. Trimble The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S |
author_facet |
David B. En Eld Alberto M. Mestas-nu~nez Paul J. Trimble |
author_sort |
David B. En Eld |
title |
The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S |
title_short |
The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S |
title_full |
The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S |
title_fullStr |
The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S |
title_full_unstemmed |
The Atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental U.S |
title_sort |
atlantic multidecadal oscillation and its relation to rainfall and river fl ows in the continental u.s |
publishDate |
2001 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.6168 http://www.aoml.noaa.gov/phod/docs/enfield/enfield_etal2001.pdf |
long_lat |
ENVELOPE(65.633,65.633,-70.433,-70.433) ENVELOPE(24.179,24.179,65.691,65.691) |
geographic |
Kerr Posi |
geographic_facet |
Kerr Posi |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://www.aoml.noaa.gov/phod/docs/enfield/enfield_etal2001.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.586.6168 http://www.aoml.noaa.gov/phod/docs/enfield/enfield_etal2001.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766123666514378752 |