The air and
snow surface temperatures warm when storm clouds pass over the site, acting as a blanket that traps heat, and then they gradually cool as heat radiates to space after skies clear.
Not exact matches
Sea ice and
snow cover loss create a feedback look that can accelerate global
warming; with fewer reflective
surfaces on the planet, more sunlight can thereby be absorbed, driving
surface temperatures even higher, the scientists explained.
Invasive species are entering the region with or without shipping, says Ted Scambos of the National
Snow and Ice Data Center in Colorado;
warming of the Arctic Ocean's
surface temperatures has already increased mixing with foreign waters and all the microbes they contain.
The study marks the first time that human influence on the climate has been demonstrated in the water cycle, and outside the bounds of typical physical responses such as
warming deep ocean and sea
surface temperatures or diminishing sea ice and
snow cover extent.
Consistent with observed changes in
surface temperature, there has been an almost worldwide reduction in glacier and small ice cap (not including Antarctica and Greenland) mass and extent in the 20th century;
snow cover has decreased in many regions of the Northern Hemisphere; sea ice extents have decreased in the Arctic, particularly in spring and summer (Chapter 4); the oceans are
warming; and sea level is rising (Chapter 5).
Re 9 wili — I know of a paper suggesting, as I recall, that enhanced «backradiation» (downward radiation reaching the
surface emitted by the air / clouds) contributed more to Arctic amplification specifically in the cold part of the year (just to be clear, backradiation should generally increase with any
warming (aside from greenhouse feedbacks) and more so with a
warming due to an increase in the greenhouse effect (including feedbacks like water vapor and, if positive, clouds, though regional changes in water vapor and clouds can go against the global trend); otherwise it was always my understanding that the albedo feedback was key (while sea ice decreases so far have been more a summer phenomenon (when it would be
warmer to begin with), the heat capacity of the sea prevents much
temperature response, but there is a greater build up of heat from the albedo feedback, and this is released in the cold part of the year when ice forms later or would have formed or would have been thicker; the seasonal effect of reduced winter
snow cover decreasing at those latitudes which still recieve sunlight in the winter would not be so delayed).
So if you say «
snow cover in 49 states is due to more moisture in the air from global
warming» — then you have absolutely no idea WTF you are talking about.The air is not
warm, and Sea
Surface Temperatures are also running well below normal.
Combine the satellite trend with the
surface observations and the umpteen non-
temperature based records that reflect
temperature change (from glaciers to phenology to lake freeze dates to
snow - cover extent in spring & fall to sea level rise to stratospheric temps) and the evidence for recent gradual
warming is, well, unequivocal.
The fact that AWS stations are likely to show a
warming bias compared to manned stations (as the distance between the sensor and the
snow surface tends to decrease over time, and Antarctica shows a strong
temperature gradient between the nominal 3m sensor height and the
snow surface) matters.
Global
warming leads to rising
temperatures of the oceans and the earth»
surface causing melting of polar ice caps, rise in sea levels and also unnatural patterns of precipitation such as flash floods, excessive
snow or desertification.
I agree that reduction in
snow or ice cover resulting from
warming constitutes a likely slow positive feedback, but its magnitude may be quite small, at least for the modest changes in
surface temperature that can be expected to arise if sensitivity is in fact fairly low, so the Forster / Gregory 06 results may nevertheless be a close approximation to a measurement of equilibrium climate sensitivity.
The average
surface air
temperature for the year ending September 2017 is the 2nd
warmest since 1900; however, cooler spring and summer
temperatures contributed to a rebound in
snow cover in the Eurasian Arctic, slower summer sea ice loss, and below - average melt extent for the Greenland ice sheet.