Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 유창현 | * |
dc.date.accessioned | 2019-11-22T16:30:13Z | - |
dc.date.available | 2019-11-22T16:30:13Z | - |
dc.date.issued | 2014 | * |
dc.identifier.issn | 0894-8755 | * |
dc.identifier.issn | 1520-0442 | * |
dc.identifier.other | OAK-25684 | * |
dc.identifier.uri | https://dspace.ewha.ac.kr/handle/2015.oak/252196 | - |
dc.description.abstract | An increase in the poleward heat or energy transport is often ascribed to a strengthening of the equator-to-pole gradient in temperature or in the top-of-the-atmosphere (TOA) net radiation. While this attribution conforms to the well-established flux gradient relationship, a counterexample is shown here, demonstrating that a forced atmospheric circulation, triggered by enhanced convection over the western tropical Pacific warm pool and suppressed convection over the eastern tropical Pacific and Indian Oceans, can cause the equator-to-pole gradient in the TOA net radiation to increase. | * |
dc.language | English | * |
dc.publisher | AMER METEOROLOGICAL SOC | * |
dc.title | On the Causal Relationship between Poleward Heat Flux and the Equator-to-Pole Temperature Gradient: A Cautionary Tale | * |
dc.type | Article | * |
dc.relation.issue | 17 | * |
dc.relation.volume | 27 | * |
dc.relation.index | SCIE | * |
dc.relation.index | SCOPUS | * |
dc.relation.startpage | 6519 | * |
dc.relation.lastpage | 6525 | * |
dc.relation.journaltitle | JOURNAL OF CLIMATE | * |
dc.identifier.doi | 10.1175/JCLI-D-14-00236.1 | * |
dc.identifier.wosid | WOS:000341281800009 | * |
dc.author.google | Lee, Sukyoung | * |
dc.author.google | Yoo, Changhyun | * |
dc.contributor.scopusid | 유창현(7201746369) | * |
dc.date.modifydate | 20240322114120 | * |