Not exact matches
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).
Even the
small amount of heat involved
in pasteurization
decreases the whey protein concentration of milk, but ultra-high
temperature (UHT) pasteurization and sterilization cause the worst declines.
Droplets can persist for months to years leading to
small decreases in global atmospheric
temperatures.
It could be
smaller than that or larger, depending on the way that
temperature varies with height; but it will not be larger than twice that, provided that a temporary saturation doesn't happen and then significantly reverse
in the span of a single doubling —
in other words, provided that the process of any temporary saturation and following reversal (wherein BTc0 increases, halts, and then
decreases, or
in the opposite order) can be sufficiently resolved by the fractional change
in CO2.
The relative simplicity of the curve of the long - term data — a
decrease in temperature from the late 19th to the early 20th centuries, followed by a relatively steady increase to present — is extremely unusual for such a
small area of the globe.
As for how this could be — and
in light of the findings of the references listed above — Rankl et al. reasoned that «considering increasing precipitation
in winter and
decreasing summer mean and minimum
temperatures across the upper Indus Basin since the 1960s,» plus the «short response times of
small glaciers,» it is only logical to conclude that these facts «suggest a shift from negative to balanced or positive mass budgets
in the 1980s or 1990s or even earlier, induced by changing climatic conditions since the 1960s.»
While SO2 emissions may have had some
small role
in that period, they can't have a role
in the current standstill, as the increase of emissions
in SE Asia is compensated by the
decrease in emissions
in the Western world, thus there is hardly any increase
in cooling aerosols while CO2 levels are going up at record speed and
temperatures are stalled.
And while
temperature should
decrease the total amount of carbon
in the upper layer of the oceans, we see an increase
in carbon (and a
decrease in 13C / 12C ratio)- Ice cores, tree carbon and coralline sponges all give
small 13C / 12C variations over the Holocene, but all show a steady and ever faster decline since about 1850.
Recent trends
in the mid - and low latitude foE and foF1 are a slight increase, and
in foF2
in day - time a very
small decrease, probably due to changes
in minor constituent chemistry and various
temperature - dependent reactions and loss rates.
That has now switched, and the
small decrease in the global
temperature between about 2002 and 2008 seems to reflect that.
Mike, I have long felt that a
decrease in cloudiness better explains such things as glacier retreat than the
small increase
in global average
temperature.