FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2065994780> ?p ?o ?g. }

• W2065994780 endingPage "4980" @default.
• W2065994780 startingPage "4962" @default.
• W2065994780 abstract "Abstract The seasonal cycle of the heating of the atmosphere is divided into a component due to direct solar absorption in the atmosphere and a component due to the flux of energy from the surface to the atmosphere via latent, sensible, and radiative heat fluxes. Both observations and coupled climate models are analyzed. The vast majority of the seasonal heating of the northern extratropics (78% in the observations and 67% in the model average) is due to atmospheric shortwave absorption. In the southern extratropics, the seasonal heating of the atmosphere is entirely due to atmospheric shortwave absorption in both the observations and the models, and the surface heat flux opposes the seasonal heating of the atmosphere. The seasonal cycle of atmospheric temperature is surface amplified in the northern extratropics and nearly barotropic in the Southern Hemisphere; in both cases, the vertical profile of temperature reflects the source of the seasonal heating. In the northern extratropics, the seasonal cycle of atmospheric heating over land differs markedly from that over the ocean. Over the land, the surface energy fluxes complement the driving absorbed shortwave flux; over the ocean, they oppose the absorbed shortwave flux. This gives rise to large seasonal differences in the temperature of the atmosphere over land and ocean. Downgradient temperature advection by the mean westerly winds damps the seasonal cycle of heating of the atmosphere over the land and amplifies it over the ocean. The seasonal cycle in the zonal energy transport is 4.1 PW. Finally, the authors examine the change in the seasonal cycle of atmospheric heating in 11 models from phase 3 of the Coupled Model Intercomparison Project (CMIP3) due to a doubling of atmospheric carbon dioxide from preindustrial concentrations. The seasonal heating of the troposphere is everywhere enhanced by increased shortwave absorption by water vapor; it is reduced where sea ice has been replaced by ocean, which increases the effective heat storage reservoir of the climate system and thereby reduces the seasonal magnitude of energy fluxes between the surface and the atmosphere. As a result, the seasonal amplitude of temperature increases in the upper troposphere (where atmospheric shortwave absorption increases) and decreases at the surface (where the ice melts)." @default.
• W2065994780 created "2016-06-24" @default.
• W2065994780 creator A5066043050 @default.
• W2065994780 creator A5072873428 @default.
• W2065994780 date "2013-07-12" @default.
• W2065994780 modified "2023-10-18" @default.
• W2065994780 title "The Seasonal Cycle of Atmospheric Heating and Temperature" @default.
• W2065994780 cites W1609650847 @default.
• W2065994780 cites W1969583657 @default.
• W2065994780 cites W1976069398 @default.
• W2065994780 cites W1984962847 @default.
• W2065994780 cites W2014537219 @default.
• W2065994780 cites W2018870291 @default.
• W2065994780 cites W2031675273 @default.
• W2065994780 cites W2043015466 @default.
• W2065994780 cites W2056903736 @default.
• W2065994780 cites W2060614081 @default.
• W2065994780 cites W2061291627 @default.
• W2065994780 cites W2062217294 @default.
• W2065994780 cites W2073401570 @default.
• W2065994780 cites W2073773661 @default.
• W2065994780 cites W2079826691 @default.
• W2065994780 cites W2081409711 @default.
• W2065994780 cites W2083070320 @default.
• W2065994780 cites W2088390370 @default.
• W2065994780 cites W2091778155 @default.
• W2065994780 cites W2098585742 @default.
• W2065994780 cites W2099551720 @default.
• W2065994780 cites W2108123321 @default.
• W2065994780 cites W2111828678 @default.
• W2065994780 cites W2112964373 @default.
• W2065994780 cites W2122511023 @default.
• W2065994780 cites W2135028770 @default.
• W2065994780 cites W2141748334 @default.
• W2065994780 cites W2153815268 @default.
• W2065994780 cites W2163679184 @default.
• W2065994780 cites W2163830001 @default.
• W2065994780 cites W2172400319 @default.
• W2065994780 cites W2174335611 @default.
• W2065994780 cites W2177650163 @default.
• W2065994780 doi "https://doi.org/10.1175/jcli-d-12-00713.1" @default.
• W2065994780 hasPublicationYear "2013" @default.
• W2065994780 type Work @default.
• W2065994780 sameAs 2065994780 @default.
• W2065994780 citedByCount "56" @default.
• W2065994780 countsByYear W20659947802013 @default.
• W2065994780 countsByYear W20659947802014 @default.
• W2065994780 countsByYear W20659947802016 @default.
• W2065994780 countsByYear W20659947802017 @default.
• W2065994780 countsByYear W20659947802018 @default.
• W2065994780 countsByYear W20659947802019 @default.
• W2065994780 countsByYear W20659947802020 @default.
• W2065994780 countsByYear W20659947802021 @default.
• W2065994780 countsByYear W20659947802022 @default.
• W2065994780 countsByYear W20659947802023 @default.
• W2065994780 crossrefType "journal-article" @default.
• W2065994780 hasAuthorship W2065994780A5066043050 @default.
• W2065994780 hasAuthorship W2065994780A5072873428 @default.
• W2065994780 hasBestOaLocation W20659947801 @default.
• W2065994780 hasConcept C121332964 @default.
• W2065994780 hasConcept C127313418 @default.
• W2065994780 hasConcept C153294291 @default.
• W2065994780 hasConcept C153385146 @default.
• W2065994780 hasConcept C178790620 @default.
• W2065994780 hasConcept C185592680 @default.
• W2065994780 hasConcept C19369268 @default.
• W2065994780 hasConcept C205649164 @default.
• W2065994780 hasConcept C2776272892 @default.
• W2065994780 hasConcept C2778835443 @default.
• W2065994780 hasConcept C39432304 @default.
• W2065994780 hasConcept C49204034 @default.
• W2065994780 hasConcept C5072599 @default.
• W2065994780 hasConcept C58024561 @default.
• W2065994780 hasConcept C59242433 @default.
• W2065994780 hasConcept C62520636 @default.
• W2065994780 hasConcept C65440619 @default.
• W2065994780 hasConcept C68709404 @default.
• W2065994780 hasConcept C74902906 @default.
• W2065994780 hasConcept C91586092 @default.
• W2065994780 hasConcept C97355855 @default.
• W2065994780 hasConceptScore W2065994780C121332964 @default.
• W2065994780 hasConceptScore W2065994780C127313418 @default.
• W2065994780 hasConceptScore W2065994780C153294291 @default.
• W2065994780 hasConceptScore W2065994780C153385146 @default.
• W2065994780 hasConceptScore W2065994780C178790620 @default.
• W2065994780 hasConceptScore W2065994780C185592680 @default.
• W2065994780 hasConceptScore W2065994780C19369268 @default.
• W2065994780 hasConceptScore W2065994780C205649164 @default.
• W2065994780 hasConceptScore W2065994780C2776272892 @default.
• W2065994780 hasConceptScore W2065994780C2778835443 @default.
• W2065994780 hasConceptScore W2065994780C39432304 @default.
• W2065994780 hasConceptScore W2065994780C49204034 @default.
• W2065994780 hasConceptScore W2065994780C5072599 @default.
• W2065994780 hasConceptScore W2065994780C58024561 @default.
• W2065994780 hasConceptScore W2065994780C59242433 @default.
• W2065994780 hasConceptScore W2065994780C62520636 @default.
• W2065994780 hasConceptScore W2065994780C65440619 @default.
• W2065994780 hasConceptScore W2065994780C68709404 @default.

• next