One side of the Oasis
thinner than its opposite edge, and yet the thickest side is thinner than any of the other Kindle versions.
Not exact matches
Somewhere in between these two
opposite poles you have good defenders who would be easier and cheaper to sign
than the Dortmund star while still being able to significantly add to our paper
thin defensive options.
It was long and
thin, and the rows of teeth on
opposite sides were nearly parallel — more like an Australopithecus's jaw
than a human's rounder one.
While previous scaling laws predicted that humans» brains would be more resilient to blasts
than animals», Radovitzky's team found the
opposite: that in fact, humans are much more vulnerable, as they have
thinner skulls to protect much larger brains.
Warming must occur below the tropopause to increase the net LW flux out of the tropopause to balance the tropopause - level forcing; there is some feedback at that point as the stratosphere is «forced» by the fraction of that increase which it absorbs, and a fraction of that is transfered back to the tropopause level — for an optically thick stratosphere that could be significant, but I think it may be minor for the Earth as it is (while CO2 optical thickness of the stratosphere alone is large near the center of the band, most of the wavelengths in which the stratosphere is not transparent have a more moderate optical thickness on the order of 1 (mainly from stratospheric water vapor; stratospheric ozone makes a contribution over a narrow wavelength band, reaching somewhat larger optical thickness
than stratospheric water vapor)(in the limit of an optically
thin stratosphere at most wavelengths where the stratosphere is not transparent, changes in the net flux out of the stratosphere caused by stratospheric warming or cooling will tend to be evenly split between upward at TOA and downward at the tropopause; with greater optically thickness over a larger fraction of optically - significant wavelengths, the distribution of warming or cooling within the stratosphere will affect how such a change is distributed, and it would even be possible for stratospheric adjustment to have
opposite effects on the downward flux at the tropopause and the upward flux at TOA).
There's practically always more IR emission from the
thin layer
than absorption (in exceptional cases the air might be so warm that the
opposite is true).