| dc.contributor.author | Anna Lea Albright | |
| dc.contributor.author | Sandrine Bony | |
| dc.contributor.author | Bjorn Stevens | |
| dc.contributor.author | Raphaela Vogel | |
| dc.date.accessioned | 2023-04-12T18:32:14Z | |
| dc.date.available | 2023-04-12T18:32:14Z | |
| dc.date.copyright | 2022/09/01 | |
| dc.date.issued | 2022 | |
| dc.identifier.other | JAS-D-21-0337.1.pdf | |
| dc.identifier.uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4289838 | |
| dc.description.abstract | The trade wind subcloud layer is an important structural component of the atmosphere. Its thermodynamic variability has long been characterized using simple frameworks, of which mixed-layer theory is the simplest kind. Past studies qualitatively support such a description, yet the adequacy of mixed-layer theory as a quantitative description has not been tested. Here we use observations collected during the Elucidating the Role of Clouds–Circulation Coupling in Climate (EUREC | |
| dc.publisher | American Meteorological Society | |
| dc.title | Observed Subcloud-Layer Moisture and Heat Budgets in the Trades | |
| dc.type | Journal Paper | |
| dc.journal.volume | 79 | |
| dc.journal.issue | 9 | |
| dc.journal.title | Journal of the Atmospheric Sciences | |
| dc.identifier.doi | 10.1175/JAS-D-21-0337.1 | |
| dc.journal.fristpage | 2363 | |
| dc.journal.lastpage | 2385 | |
| dc.page | 2363–2385 | |
| dc.tree | Journal of the Atmospheric Sciences:;2022:;volume( 079 ):;issue: 009 | |
| dc.contenttype | Fulltext | |
