The warm early - Holocene climate around Svalbard was driven primarily
by higher insolation and greater influx of warm Atlantic Water, but feedback processes further influenced the regional climate.»
Not exact matches
A recent study on the GIS melt during the Eemian argues that temperature rise alone produced 55 % of the melt and the rest was caused
by higher solar
insolation and feedbacks.
For instance, the commentary piece
by Eric Wolff references earlier deglaciations and points out that solar
insolation may have increased in the boreal summer during the most recent event, but was still not as
high as during previous deglacial intervals.
Ice ages are generally triggered
by minima in
high - latitude NH summer
insolation, enabling winter snowfall to persist through the year and therefore accumulate to build NH glacial ice sheets.
Similarly, times with especially intense
high - latitude NH summer
insolation, determined
by orbital changes, are thought to trigger rapid deglaciations, associated climate change and sea level rise.
The rapid 1940s retreat is linked to unusually
high solar
insolation and patterns of precipitation governed
by the Atlantic Multidecadal and North Atlantic Oscillation.42, 43
Then that lowest atmosphere layer emit and a 50 - 50 split sends it half up and half down; and the up ward is again absorbed
by a
higher and now cooler layer; which in turn emits but now at a lower temperature; until finally some much
higher and much cooler layer gets to emit radiation that actually escapes to space and that radiating temperature is the one that must balance with the incoming TSI
insolation rate.
In the case of the 100 kyr ice age cycles, that forcing is
high northern latitude summer
insolation driven
by predictable changes in Earth's orbital and rotational parameters — aka, Milankovitch theory — which has the intial effect of melting glaciers, thereby reducing albedo at those latitudes.
Regardless of the carbon source (s), it has been shown that the hyperthermals were astronomically paced, spurred
by coincident maxima in the Earth's orbit eccentricity and spin axis tilt [17], which increased
high - latitude
insolation and warming.
When the greenhouse gas reradiates this LR radiation, some radiates back towards the surface which then heats up — to a
higher temperature than caused
by the initial
insolation, and an increase in the thermal energy within the surface.
«The Milankovitch theory of climate change proposes that glacial - interglacial cycles are driven
by changes in summer
insolation at
high northern latitudes [i.e., solar irradiance received].