%0 Journal Article
%T mid-latitudeatmosphericresponsestoheatandvorticityforcingusingalinearbaroclinicmodel
%A QIU
%A Shuang£¿
%A FANG
%A Jiabei£¿
%A YANG
%A Xiuqun£¿
%J ÆøÏó¿Æѧ
%P 149-161
%D 2014
%R 10.3969/2013jms.0060
%X basedondiagnosticanalysisofreanalysisdatafor58-year,thedistributioncharacteristicsofdecadalvariabilityindiabaticheating,transienteddyheatingandtransienteddyvorticityforcingrelatedtotheseasurfacetemperature(sst)anomaliesoverthenorthpacific,aswellastheirrelationshipwithanomalousatmosphericcirculationhavebeeninvestigatedinthispaper.alinearbaroclinicmodel(lbm)wasusedtoinvestigateatmosphericresponsestoidealizedandrealisticheatandvorticityforcinganomalies,andthentocomparerelativerolesofdifferentkindsofforcingintermsofgeopotentialheightresponses.theresultsillustratethattheresponsesofatmosphericheightfieldstothemid-latitudeheatingcanbeeitherbaroclinicorbarotropic.theresponsestructureissensitivetotherelativehorizontallocationofheatingwithrespecttothebackgroundjetflow,aswellastotheverticalprofileofheating.theresponsetotheidealizeddeepheatingovertheeasternnorthpacific,mimickingtheobservedheatinganomaly,isbaroclinic.theatmosphericresponsetothemid-latitudevorticityforcingisalwaysbarotropic,resultinginageopotentiallowthatisinphasewiththeforcing.theatmosphericresponsestotherealisticheatandvorticityforcingshowthesimilarresults,suggestingthatdiabaticheating,transienteddyheatingandtransienteddyvorticityforcingcanallcauseatmosphericanomaliesandthatthevorticityforcingplaysarelativelymoreimportantroleinmaintainingtheequivalent-barotropicstructureofgeopotentialheightanomalies.
%K diabatic
%K heating
%K transient
%K eddy
%K heating
%K transient
%K eddy
%K vorticity
%K forcing
%K linear
%K baroclinic
%K model
%U http://www.jms1980.com/ch/reader/view_abstract.aspx?file_no=20140204&flag=1