Open AccessMomentum budget of the atmospheric boundary layer over the Greenland ice sheet and its surrounding seas
Author(s) -
van Angelen J. H.,
van den Broeke M. R.,
van de Berg W. J.
Publication year - 2011
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2010jd015485
Subject(s) - katabatic wind , ice sheet , geology , antarctic sea ice , ice stream , climatology , sea ice , arctic ice pack , future sea level , atmospheric circulation , forcing (mathematics) , ice shelf , antarctic ice sheet , cryosphere , drift ice , atmospheric sciences , oceanography
The atmospheric circulation patterns over the Greenland ice sheet and its surrounding seas are studied by explicitly calculating the momentum budget components, using data of a high‐resolution regional atmospheric climate model. In winter (DJF), the katabatic pressure gradient force (PGF) dominates the momentum budget of the atmospheric boundary layer (ABL) over the ice sheet. Over the western slopes of the ice sheet, the large‐scale PGF acts in the same direction as the katabatic PGF, resulting in a strong southerly jet of up to 12 m s −1 . In winter, the accumulation of cold air over the sea ice along the northeast coast leads to a thermally induced northerly flow. This circulation facilitates southward sea ice transport in this area and is enhanced by the large‐scale circulation. Along the west coast, a similar west‐east temperature gradient also forces a northerly flow. In the summer months, sea ice is absent, and thermal wind forcing is largely reduced over the ocean. Summer insolation also reduces katabatic forcing; the large‐scale forcing dominates the ABL momentum budget over the ice sheet. Heating of the ABL over the snow‐free tundra induces thermal contrasts with the ice sheet and ocean, forcing barrier winds in the coastal regions. Throughout the year, strong surface layer winds along the southeast coast of Greenland are forced by the large‐scale PGF.