A third effect occurs when black carbon (BC) particles land on snow, and the tiny specks of dark material in
the upper snow layers absorb heat from the sun and promote melting.
Not exact matches
For each measurement, they lowered a marine
snow catcher beneath the
upper layer of the ocean to capture a water sample.
In the picture above, there is a lot of very dirty
snow in the
upper layers.
For example, the lower atmosphere and the
upper layers of the ocean have also warmed,
snow and ice cover are decreasing in the Northern Hemisphere, the Greenland ice sheet is shrinking, and sea level is rising (see Figure 1b).
Based on the understanding of both the physical processes that control key climate feedbacks (see Section 8.6.3), and also the origin of inter-model differences in the simulation of feedbacks (see Section 8.6.2), the following climate characteristics appear to be particularly important: (i) for the water vapour and lapse rate feedbacks, the response of
upper - tropospheric RH and lapse rate to interannual or decadal changes in climate; (ii) for cloud feedbacks, the response of boundary -
layer clouds and anvil clouds to a change in surface or atmospheric conditions and the change in cloud radiative properties associated with a change in extratropical synoptic weather systems; (iii) for
snow albedo feedbacks, the relationship between surface air temperature and
snow melt over northern land areas during spring and (iv) for sea ice feedbacks, the simulation of sea ice thickness.