Your browser doesn't support javascript.
loading
Snow on Arctic Sea Ice in a Warming Climate as Simulated in CESM.
Webster, M A; DuVivier, A K; Holland, M M; Bailey, D A.
Afiliación
  • Webster MA; Geophysical Institute University of Alaska Fairbanks Fairbanks AK USA.
  • DuVivier AK; National Center for Atmospheric Research Boulder CO USA.
  • Holland MM; National Center for Atmospheric Research Boulder CO USA.
  • Bailey DA; National Center for Atmospheric Research Boulder CO USA.
J Geophys Res Oceans ; 126(1): e2020JC016308, 2021 Jan.
Article en En | MEDLINE | ID: mdl-33842183
Earth system models are valuable tools for understanding how the Arctic snow-ice system and the feedbacks therein may respond to a warming climate. In this analysis, we investigate snow on Arctic sea ice to better understand how snow conditions may change under different forcing scenarios. First, we use in situ, airborne, and satellite observations to assess the realism of the Community Earth System Model (CESM) in simulating snow on Arctic sea ice. CESM versions one and two are evaluated, with V1 being the Large Ensemble experiment (CESM1-LE) and V2 being configured with low- and high-top atmospheric components. The assessment shows CESM2 underestimates snow depth and produces overly uniform snow distributions, whereas CESM1-LE produces a highly variable, excessively-thick snow cover. Observations indicate that snow in CESM2 accumulates too slowly in autumn, too quickly in winter-spring, and melts too soon and rapidly in late spring. The 1950-2050 trends in annual mean snow depths are markedly smaller in CESM2 (-0.8 cm decade-1) than in CESM1-LE (-3.6 cm decade-1) due to CESM2 having less snow overall. A perennial, thick sea-ice cover, cool summers, and excessive summer snowfall facilitate a thicker, longer-lasting snow cover in CESM1-LE. Under the SSP5-8.5 forcing scenario, CESM2 shows that, compared to present-day, snow on Arctic sea ice will: (1) undergo enhanced, earlier spring melt, (2) accumulate less in summer-autumn, (3) sublimate more, and (4) facilitate marginally more snow-ice formation. CESM2 also reveals that summers with snow-free ice can occur ∼30-60 years before an ice-free central Arctic, which may promote faster sea-ice melt.
Palabras clave

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Tipo de estudio: Prognostic_studies Idioma: En Revista: J Geophys Res Oceans Año: 2021 Tipo del documento: Article Pais de publicación: Estados Unidos

Texto completo: 1 Colección: 01-internacional Base de datos: MEDLINE Tipo de estudio: Prognostic_studies Idioma: En Revista: J Geophys Res Oceans Año: 2021 Tipo del documento: Article Pais de publicación: Estados Unidos