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dc.contributor.authorMaliekal, Jose
dc.date.accessioned2021-09-07T17:37:58Z
dc.date.available2021-09-07T17:37:58Z
dc.date.issued1998-06-15
dc.identifier.citationMaliekal, J.A., (1998) Feedback relations and causal orders between sea surface temperature and convection within the western Pacific warm pool, Geophysical Research Letters, VOL. 25, NO.12, PAGES 2193-2196, JUNE 15,1998
dc.identifier.urihttp://hdl.handle.net/20.500.12648/2190
dc.description“An edited version of this paper was published by AGU. Copyright 1998 American Geophysical Union.”
dc.description.abstractAnalysis of time series of standardized anomalies of sea surface temperature and outgoing longwave radiation from the western Pacific warm pool revealed two distinct modes of atmosphere-ocean interaction. A statistically binding positive feedback relationship between convection and ocean temperature exists over the equatorial region surrounding the international date line. Here, the contemporaneous feedback between the/se two variables is not statistically significant. A causal order from the ocean temperature to outgoing longwave radiation is detected in a region of the Southwest Pacific, where ocean patches with temperatures greater than or equal to 29.75° C form most frequently. Dynamical implications associated with the aforementioned feedback relationship and causal order are illustrated by estimating the impact of a sudden transient LTJ.crease in convection on future values of sea surface temperature and vice versa.
dc.titleFeedback relations and causal orders between sea surface temperature and convection within the western Pacific warm pool
dc.typearticle
dc.source.journaltitleGeophysical Research Letters
dc.source.volume25
dc.source.issue12
refterms.dateFOA2021-09-07T17:37:58Z
dc.description.institutionSUNY Brockport
dc.source.peerreviewedTRUE
dc.source.statuspublished
dc.description.publicationtitleEarth Sciences Faculty Publications
dc.contributor.organizationThe College at Brockport
dc.languate.isoen_US


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