The pattern is clear: Wing length has decreased «significantly» in
response to warmer summers.
We find that most peat - forming ecosystems have initiated since 2800 cal BP, in
response to warmer summers and increasing summer insolation.
Not exact matches
Pinsky will examine this further with
summer flounder, a popular east coast sport fish, as populations drop off the coast of the Carolinas in
response to warmer waters and increase off the Mid-Atlantic States.
Mountain pine beetle develops an unprecedented
summer generation in
response to climate
warming.
[
Response: Those ice shelves are just south of James Ross Island, and collapsed due
to summer warming.
[
Response: Sea ice is still not at levels seen during the Early Holocene, and since we are discussing sea floor sediments the main reason given
to be concerned is that the change of
summer sea ice will
warm the bottom sea water, we are clearly not there yet.
(57j) For surface + tropospheric
warming in general, there is (given a cold enough start) positive surface albedo feedback, that is concentrated at higher latitudes and in some seasons (though the temperature
response to reduced
summer sea ice cover tends
to be realized more in winter when there is more heat that must be released before ice forms).
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).
I understand the concept of
summer to winter variation being a global
warming response but the net change should be negative — and its not!
With the late -
summer ice edge located farther north than it used
to be, storms produce larger waves and more coastal erosion.5 An additional contributing factor is that coastal bluffs that were «cemented» by ice - rich permafrost are beginning
to thaw in
response to warmer air and ocean waters, and are therefore more vulnerable
to erosion.22 Standard defensive adaptation strategies
to protect coastal communities from erosion, such as use of rock walls, sandbags, and riprap, have been largely unsuccessful.23 Several coastal communities are seeking
to relocate
to escape erosion that threatens infrastructure and services but, because of high costs and policy constraints on use of federal funds for community relocation, only one Alaskan village has begun
to relocate (see also Ch.
[
Response: Your argument misses the point in three different and important ways, not even considering whether or not the Black Hills data have any general applicability elsewhere, which they may or may not: (1) It ignores the point made in the post about the potential effect of previous, seasonal
warming on the magnitude of an extreme event in mid
summer to early fall, due
to things like (especially) a depletion in soil moisture and consequent accumulation of degree days, (2) it ignores that biological sensitivity is far FAR greater during the
warm season than the cold season for a whole number of crucial variables ranging from respiration and photosynthesis
to transpiration rates, and (3) it ignores the potential for derivative effects, particularly fire and smoke, in radically increasing the local temperature effects of the heat wave.