Stabilising CO2 concentrations in
the atmosphere at any given level, already at 393 parts per million and rising at an average 2.3 ppm per year, requires annual emission be reduced more than 80 per cent below current levels eventually.
Not exact matches
However, even
at the temperature of its dayside, its
atmosphere probably resembles the molecule - dominated
atmospheres of other planets and,
given the
level of ultraviolet irradiation it experiences, its
atmosphere is unlikely to be substantially ablated over the lifetime of its star.
From day one we've been committed to providing a welcoming
atmosphere so that guests feel right
at home and we always endeavor to treat our patrons with the same
level of integrity, kindness and respect that we
give to our own friends and family.
[note1] To a good approximation, the pressure
at any
given vertical
level in the
atmosphere is such that it supports the weight of the column of gasses above it.
At a
given level in the
atmosphere, any low that is generally characterized by colder air near its center than around its periphery; the opposite of a warm low.
A stronger gravitational field will produce a lower, denser, warmer surface than a weaker gravitational field since the amount of solar energy retained by the
atmosphere will be focused into a smaller volume and that amount of energy will be determined by the amount of mass available to absorb it
at any
given level of solar irradiation.
I think that all they represent is the temperature of the
atmosphere when it is in equilibrium
at any
given level.
-- higher temperatures
give more CO2 from the oceans which, even after fractionation
at the sea surface, has a higher d13C
level than the current
atmosphere.
Bolin & Eriksson's «buffer» factor would
give about 10 times higher CO2 concentration in air vs. sea water
at about 0.0003
atmospheres CO2 partial pressure, increasing dramatically to an air / water CO2 partition coefficient of about 50:1
at a CO2 partial pressure of about 0.003
atmospheres (10 times the assumed pre-industrial
level; Bacastow & Keeling, 1973; see Section 7 below for more on the «buffer» factor).
The presence of feedback effects and tipping points calls into question some of the most fundamental assumptions of climate change negotiations, including the belief that we can «overshoot» to, say, 550 ppm and then work back to 450 ppm (the path advocated in the Stern and Garnaut reports), that greenhouse gas concentrations in the
atmosphere can be stabilised
at some
level, and the belief that we can adapt to some
given degree of warming.
Given that the oceans drive the
atmosphere and the oceans are running
at record OHC
levels, this is not surprising.
As current
levels of CO2 show the same CO2
levels at the south pole as for the rest (95 %) of the
atmosphere within a year (despite fast changes in
level), that
gives confidence that ice cores show more or less global CO2
levels of ancient
atmospheres...
Furthermore, the term climate and its measurement (mean world - wide temperature or mwwT) as a temperature
level is really a measure of total eK stored within the earth's entire
atmosphere at any
given moment.
ii) In the case of the Ideal Gas Law it is the height of an
atmosphere of a
given mass that determines the number of molecules per unit of volume
at the surface and the more molecules per unit of volume the hotter the surface will become
at a
given level of solar input.
In the case of GGR, we have started to see a shift, e.g., with a major programme funded by the UK National Environment Research Council (NERC) that «will undertake research to improve our knowledge of the options for removing carbon dioxide (CO2) and other greenhouse gases from the
atmosphere at a climatically - relevant scale,
giving interdisciplinary attention to the environmental, technical, economic, governance and wider societal aspects of such approaches on a national
level and in an international context» (http://www.nerc.ac.uk/research/funded/programmes/ggr/).
I believe the IPCC plans all call for a black box solution where we develop a technology to remove carbon dioxide from the
atmosphere or ocean to drive the CO2
levels or to
at least slow the rise of CO2 and
give us more time to make fundamental changes in the way we live to limit global warming to some arbitrary
level.
Should the climate negotiations try to cap CO2 pollution in the
atmosphere at 550 parts per million (ppm), 450 ppm, or some other (hopefully lower) figure Or should we take an entirely different approach and try to cap temperature change itself, rather than CO2 pollution And what must we know about the kinds of impacts and instabilities that can be expected
at any
given level View Full Text»
The horizontal blue lines
give the threshold CO2 needed to make the
atmosphere optically thick
at 1x the preindustrial CO2
level and 4x that
level.
I don't know how accurate 510 million km2 is for Earth's surface area; taking 4 * pi * 6371 ^ 2 km2 ~ = 510.064 million km2; but I don't know the formula for an ellipsoid (polar radius is slightly smaller than equatorial radius)(for what it's worth, 4 * pi * 6381 ^ 2 km2 ~ = 511.667 million km2, which
gives a sense of why most of the mass of the
atmosphere can be approximated as having the same horizontal area as
at sea
level (a 1 % increase in area is reached
at a height of about 31.8 km)-RRB-.