Zobrazeno 1 - 10
of 95
pro vyhledávání: '"Surface Heat Budget of the Arctic Ocean"'
Publikováno v:
Journal of the Atmospheric Sciences. 77:2687-2716
Climate models still have deficits in reproducing the surface energy and momentum budgets in Arctic regions. One of the reasons is that currently used transfer coefficients occurring in parameterizations of the turbulent fluxes are based on stability
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d11db515bf306f433d134e7005f93a1e
https://doi.org/10.1175/jas-d-19-0255.1
https://doi.org/10.1175/jas-d-19-0255.1
Autor:
Felix Pithan, S. Mubashshir Ali
Publikováno v:
Ali, Syed Mubashshir; Pithan, Felix (2020). Following moist intrusions into the Arctic using SHEBA observations in a Lagrangian perspective. Quarterly Journal of the Royal Meteorological Society, 146(732), pp. 3522-3533. Royal Meteorological Society 10.1002/qj.3859
Warm and moist air masses are transported into the Arctic from lower latitudes throughout the year. Especially in winter, such moist intrusions can trigger cloud formation and surface warming. While a typical cloudy state of the Arctic winter boundar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ec28921f26877f30598bdc74ace3d44b
https://boris.unibe.ch/144801/1/qj.3859.pdf
https://boris.unibe.ch/144801/1/qj.3859.pdf
Publikováno v:
Journal of Geophysical Research: Oceans. 125
Data collected by two buoy arrays that operated during the ice seasons of 2014/2015 and 2016/2017 were used to characterize annual cycles of ice motion and deformation in the western Arctic Ocean. An anomalously strong and weak Beaufort Gyre in 2014/
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b1a88ad64a517271cbe675e538ef4726
https://doi.org/10.1029/2019jc015310
https://doi.org/10.1029/2019jc015310
Autor:
Christof Lüpkes, Vladimir M. Gryanik
Publikováno v:
Boundary-Layer Meteorology. 166:301-325
In climate and weather prediction models the near-surface turbulent fluxes of heat and momentum and related transfer coefficients are usually parametrized on the basis of Monin–Obukhov similarity theory (MOST). To avoid iteration, required for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d656f4f01f32d0430946a5f9ad489875
https://doi.org/10.1007/s10546-017-0302-x
https://doi.org/10.1007/s10546-017-0302-x
Autor:
Dmitry Chechin
Publikováno v:
Atmosphere
Volume 12
Issue 5
Atmosphere, Vol 12, Iss 591, p 591 (2021)
Volume 12
Issue 5
Atmosphere, Vol 12, Iss 591, p 591 (2021)
A relationship between the friction velocity u☆ and mean wind speed U in a stable atmospheric boundary layer (ABL) over Arctic sea ice was considered. To that aim, the observations collected during the Surface Heat Budget of the Arctic Ocean (SHEBA
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c5443afed095a3ce2c6c93277681ae6
https://doi.org/10.3390/atmos12050591
https://doi.org/10.3390/atmos12050591
Publikováno v:
Climate Dynamics. 49:1341-1364
Observations from the Surface Heat Budget of the Arctic Ocean (SHEBA) project are used to describe a sequence of events linking midwinter long-range advection of atmospheric heat and moisture into the Arctic Basin, formation of supercooled liquid wat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06cf162ec51cf69e4be1bf1acc425f39
https://doi.org/10.1007/s00382-016-3383-1
https://doi.org/10.1007/s00382-016-3383-1
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 33:453-460
The accuracy of cloud-screened 2-m air temperatures derived from the intersatellite-calibrated brightness temperatures based on the High Resolution Infrared Radiation Sounder (HIRS) measurements on board the National Oceanic and Atmospheric Administr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2bcdd516b518038484b960943f19aff
https://doi.org/10.1175/jtech-d-15-0217.1
https://doi.org/10.1175/jtech-d-15-0217.1
Autor:
Edgar L. Andreas, Rachel E. Jordan
Publikováno v:
Journal of Climate. 28:6360-6380
Numerical models of the atmosphere, oceans, and sea ice are divided into horizontal grid cells that can range in size from a few kilometers to hundreds of kilometers. In these models, many surface-level variables are assumed to be uniform over a grid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8b5a706115096ffa9e8c33fa10c7cfa3
https://doi.org/10.1175/jcli-d-14-00768.1
https://doi.org/10.1175/jcli-d-14-00768.1
Publikováno v:
Journal of Climate. 27:265-272
Observations from the Surface Heat Budget of the Arctic Ocean experiment (SHEBA) suggest that the Arctic Basin is characterized by two distinctly different preferred atmospheric states during wintertime. These states appear as two peaks in the freque
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::09c3216ac533e97c5b390d66d942f822
https://doi.org/10.1175/jcli-d-13-00271.1
https://doi.org/10.1175/jcli-d-13-00271.1
Publikováno v:
Polar Research, Vol 32, Iss 0, Pp 1-18 (2013)
Polar Research; Vol 32 (2013) incl supplements
Polar Research; Vol 32 (2013) incl supplements
This study examines the modelled surface turbulent fluxes over sea ice from the bulk algorithms of the Beijing Climate Centre Climate System Model (BCC_CSM), the European Centre for Medium-Range Weather Forecasts (ECMWF) model and the Community Earth
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::be5f955b6e71c71b9a7fc062df709e8b
http://www.polarresearch.net/index.php/polar/article/download/20818/pdf_1
http://www.polarresearch.net/index.php/polar/article/download/20818/pdf_1