Specification of regional sea surface temperatures in atmospheric general circulation model simulations. Kumar, A. & Hoerling, M. P. Journal of Geophysical Research-Atmospheres, 103(D8):8901--8907, April, 1998. WOS:000073290900023doi abstract bibtex A hierarchy of atmospheric general circulation model simulations of the 1950-1994 period that employ different prescriptions of the oceanic boundary conditions are analyzed. It is demonstrated that contrary to expectations, increased spatial coverage of the sea surface temperature specification can degrade the underlying simulated climate signals. The cause for this is related to an inability to accurately model the diversity of air-sea interaction regimes that exist across the global oceans. Such failure is shown to generate spurious sources of atmospheric energy that exert global influences on interannual and decadal timescales.
@article{ kumar_specification_1998,
title = {Specification of regional sea surface temperatures in atmospheric general circulation model simulations},
volume = {103},
issn = {0747-7309},
doi = {10.1029/98JD00427},
abstract = {A hierarchy of atmospheric general circulation model simulations of the 1950-1994 period that employ different prescriptions of the oceanic boundary conditions are analyzed. It is demonstrated that contrary to expectations, increased spatial coverage of the sea surface temperature specification can degrade the underlying simulated climate signals. The cause for this is related to an inability to accurately model the diversity of air-sea interaction regimes that exist across the global oceans. Such failure is shown to generate spurious sources of atmospheric energy that exert global influences on interannual and decadal timescales.},
language = {English},
number = {D8},
journal = {Journal of Geophysical Research-Atmospheres},
author = {Kumar, A. and Hoerling, M. P.},
month = {April},
year = {1998},
note = {{WOS:000073290900023}},
keywords = {cloud, convection, enso, extratropical sst anomalies, global temperature, northern-hemisphere, ocean, pacific, roles, variability},
pages = {8901--8907}
}
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P.</span>\n\t<!-- <span class=\"bibbase_paper_year\">1998</span>. -->\n</span>\n\n\n\n<i>Journal of Geophysical Research-Atmospheres</i>,\n\n103(D8):8901--8907.\n\nApril 1998.\n\n\nWOS:000073290900023.\n\n<br class=\"bibbase_paper_content\"/>\n\n<span class=\"bibbase_paper_content\">\n \n \n \n <a href=\"javascript:showBib('kumar_specification_1998')\">\n <img src=\"http://bibbase.org/img/filetypes/bib.png\" \n\t alt=\"Specification of regional sea surface temperatures in atmospheric general circulation model simulations [bib]\" \n\t class=\"bibbase_icon\"\n\t style=\"width: 24px; height: 24px; border: 0px; vertical-align: text-top\"><span class=\"bibbase_icon_text\">Bibtex</span></a>\n \n \n\n \n \n \n \n \n\n \n <a class=\"bibbase_abstract_link\" href=\"javascript:showAbstract('kumar_specification_1998')\">Abstract</a>\n \n \n</span>\n\n<!-- -->\n<!-- <div id=\"abstract_kumar_specification_1998\"> -->\n<!-- A hierarchy of atmospheric general circulation model simulations of the 1950-1994 period that employ different prescriptions of the oceanic boundary conditions are analyzed. It is demonstrated that contrary to expectations, increased spatial coverage of the sea surface temperature specification can degrade the underlying simulated climate signals. The cause for this is related to an inability to accurately model the diversity of air-sea interaction regimes that exist across the global oceans. Such failure is shown to generate spurious sources of atmospheric energy that exert global influences on interannual and decadal timescales. -->\n<!-- </div> -->\n<!-- -->\n\n</div>\n","downloads":0,"bibbaseid":"kumar-hoerling-specificationofregionalseasurfacetemperaturesinatmosphericgeneralcirculationmodelsimulations-1998","urls":{},"role":"author","year":"1998","volume":"103","type":"article","title":"Specification of regional sea surface temperatures in atmospheric general circulation model simulations","pages":"8901--8907","number":"D8","note":"WOS:000073290900023","month":"April","language":"English","keywords":"cloud, convection, enso, extratropical sst anomalies, global temperature, northern-hemisphere, ocean, pacific, roles, variability","key":"kumar_specification_1998","journal":"Journal of Geophysical Research-Atmospheres","issn":"0747-7309","id":"kumar_specification_1998","doi":"10.1029/98JD00427","bibtype":"article","bibtex":"@article{ kumar_specification_1998,\n title = {Specification of regional sea surface temperatures in atmospheric general circulation model simulations},\n volume = {103},\n issn = {0747-7309},\n doi = {10.1029/98JD00427},\n abstract = {A hierarchy of atmospheric general circulation model simulations of the 1950-1994 period that employ different prescriptions of the oceanic boundary conditions are analyzed. It is demonstrated that contrary to expectations, increased spatial coverage of the sea surface temperature specification can degrade the underlying simulated climate signals. The cause for this is related to an inability to accurately model the diversity of air-sea interaction regimes that exist across the global oceans. Such failure is shown to generate spurious sources of atmospheric energy that exert global influences on interannual and decadal timescales.},\n language = {English},\n number = {D8},\n journal = {Journal of Geophysical Research-Atmospheres},\n author = {Kumar, A. and Hoerling, M. P.},\n month = {April},\n year = {1998},\n note = {{WOS:000073290900023}},\n keywords = {cloud, convection, enso, extratropical sst anomalies, global temperature, northern-hemisphere, ocean, pacific, roles, variability},\n pages = {8901--8907}\n}","author_short":["Kumar, A.","Hoerling, M.<nbsp>P."],"author":["Kumar, A.","Hoerling, M. P."],"abstract":"A hierarchy of atmospheric general circulation model simulations of the 1950-1994 period that employ different prescriptions of the oceanic boundary conditions are analyzed. It is demonstrated that contrary to expectations, increased spatial coverage of the sea surface temperature specification can degrade the underlying simulated climate signals. The cause for this is related to an inability to accurately model the diversity of air-sea interaction regimes that exist across the global oceans. 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