Don't know where I got my lines crossed but I herewith point out in Chapter1 figures 1.4 and 1.5, comparing
near surface temperature range observed data with projections, 1990 — 2015 with its plateau of measured data warming and large uncertainty shading.
Not exact matches
The reaction rate between atmospheric hydrogen chloride (HCl) and chlorine nitrate (ClONO2) is greatly enhanced in the presence of ice particles; HCl dissolves readily into ice, and the collisional reaction probability for ClONO2 on the
surface of ice with HCl in the mole fraction
range from ∼ 0.003 to 0.010 is in the
range from ∼ 0.05 to 0.1 for
temperatures near 200 K. Chlorine (Cl2) is released into the gas phase on a time scale of at most a few milliseconds, whereas nitric acid (HNO3), the other product, remains in the condensed phase.
Surface temperatures can
range from below freezing
near the poles to 35 °C in restricted tropical seas, while salinity can vary from 10 to 41 ppt (1.0 — 4.1 %).
Ocean acidification, rising ocean
temperatures, declining sea ice, and other environmental changes interact to affect the location and abundance of marine fish, including those that are commercially important, those used as food by other species, and those used for subsistence.16, 17,18,122,19,20,21 These changes have allowed some
near -
surface fish species such as salmon to expand their
ranges northward along the Alaskan coast.124, 125,126 In addition, non-native species are invading Alaskan waters more rapidly, primarily through ships releasing ballast waters and bringing southerly species to Alaska.5, 127 These species introductions could affect marine ecosystems, including the feeding relationships of fish important to commercial and subsistence fisheries.
We have two new entries to the long (and growing) list of papers appearing the in recent scientific literature that argue that the earth's climate sensitivity — the ultimate rise in the earth's average
surface temperature from a doubling of the atmospheric carbon dioxide content — is close to 2 °C, or
near the low end of the
range of possible values presented by the U.N.'s Intergovernmental Panel on Climate Change (IPCC).
Since the late 1970s, permafrost
temperatures across the state — including on the Seward Peninsula — have risen along with increasing air
temperatures.3, 5 In fact, 22 of 24 thaw (thermokarst) ponds studied
near Nome shrank over the latter half of the last century, with losses in
surface area
ranging from 6 to 100 percent, and averaging 55 percent.4, 8
I have, incidentally, found using a multilayer diffusive ocean model that there is a
near complete identity in the path of the model
surface temperature response to a step forcing, for the better part of a century, over a wide
range of equilibrium climate sensitivities if effective ocean diffusivity is varied to compensate.