Not exact matches
Correcting for this would result in
significant downward
adjustments over the
balance of the year, especially in the end - of - year accounting period.
The accrual
adjustments to date, especially for personal and corporate income tax revenues, are understated, which will result in
significant downward
adjustments over the
balance of the year, especially in the end - of - year accounting period.
The accrual
adjustments to date for personal and corporate income tax revenues, could be understated, which will result in
significant downward
adjustments over the
balance of the year, especially in the end - of - year accounting period.
One of the major
adjustments that the countries in non-Japan Asia have undergone in the past two years has been a
significant shift in their current account
balances.
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).
A recent paper by Graeme L. Stephens, Juilin Li, Martin Wild, Carol Anne Clayson, Norman Loeb, Seiji Kato, Tristan L'Ecuyer, Paul W. Stackhouse Jr, Matthew Lebsock & Timothy Andrews An update on Earth's energy
balance in light of the latest global observations, Nature Geoscience, 5, 691 — 696 (2012), which indicates
significant adjustments to the energy
balance MEASURED data shows how far we are from certainty.
But regardless of how these
balances are stuck, some form of country - to - country review seems likely to play a
significant role in the post-2015 climate regime, as part of a «multi-lateral
adjustment process.»
For example, utility - scale wind generation, a particularly volatile intermittent power source, requires electricity operators to make
significant adjustments to
balance generation and load, creating inefficiency in the system.