While the bulk of the new IPCC report isn't published yet, a detailed discussion of projected global warming and its anticipated effects is in the last report
(2001), including the following quote from the summary
here:
IPCC wrote:Projected adverse impacts based on models and other studies include:
* A general reduction in potential crop yields in most tropical and sub-tropical regions for most projected increases in temperature [4.2]
* A general reduction, with some variation, in potential crop yields in most regions in mid-latitudes for increases in annual-average temperature of more than a few °C [4.2]
* Decreased water availability for populations in many water-scarce regions, particularly in the sub-tropics [4.1]
* An increase in the number of people exposed to vector-borne (e.g., malaria) and water-borne diseases (e.g., cholera), and an increase in heat stress mortality [4.7]
* A widespread increase in the risk of flooding for many human settlements (tens of millions of inhabitants in settlements studied) from both increased heavy precipitation events and sea-level rise [4.5]
* Increased energy demand for space cooling due to higher summer temperatures. [4.5]
Projected beneficial impacts based on models and other studies include:
* Increased potential crop yields in some regions at mid-latitudes for increases in temperature of less than a few °C [4.2]
* A potential increase in global timber supply from appropriately managed forests [4.3]
* Increased water availability for populations in some water-scarce regions—for example, in parts of southeast Asia [4.1]
* Reduced winter mortality in mid- and high-latitudes
* Reduced energy demand for space heating due to higher winter temperatures. [4.5]
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The last report (2001)
estimated a 1.4 to 5.8 degree Celsius increase in global average temperature for 2100 compared to 1990, along with a 0.09m to 0.88m rise in sea level.
A summary part of the new 2007 report is online
here, mentioning that the best estimate for the low scenario is a 1.8 degree Celsius rise, while the best estimate for the high scenario is a 4.0 degree Celsius rise, for temperatures in 2090-2099 compared to 1980-1999. The model-based range for sea level rise excluding rapid dynamical changes in ice flow is 0.18m to 0.59m over that timeframe, from table SPM-3.
There is a lot more information even in that summary. One example is figure
SPM-7 for projected change in rainfall and other precipitation, in this case illustrating for June to August:
The above is for the A1B scenario, one with much increased future energy consumption and intermediate between a more ideal scenario eventually without much fossil fuel use (A1T) and a worse scenario remaining most fossil-fuel intensive (A1FI). And there are more scenarios considered.
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The figure above from the
preceding is a better chart than I have seen before.
If one considers "best estimate" values of the information aside from the uncertainty ranges, in W/m^2, the average source of pollution causes warming of 1.66 from carbon dioxide, 0.48 from methane (cows, etc.), 0.35 from tropospheric ozone, 0.34 from halocarbons (spray cans, etc.), and 0.33 from other warming pollution. Meanwhile, such also typically causes ~ 1.2 W/m^2 of cooling from the direct and cloud albedo effects of aerosols, plus ~ 0.05 W/m^2 of cooling from stratospheric ozone. Overall, the effect is net warming.
But notice something about the preceding. Individual sources of pollution differ from the average. For example, if a particular pollution source emitted CO2 but relatively little CH4, tropospheric ozone, halocarbons, etc. while having a proportionally larger than usual amount of aerosol emissions, it might cause much less warming than the usual polluter, possibly even net cooling in some cases.
Obviously, it is desirable to reduce pollution in general for multiple reasons. However, it is interesting to observe that factors like the CO2 to aerosol ratio may matter more for the net effect on global warming of some particular pollution sources than their CO2 emissions alone.
From the standpoint of mitigating global warming, the most effective measure might not only be to cut warming pollution but also to make up for the practical side-effect of drops in cooling aerosol pollutants by
sulphate injection or
other particulates.
Of course, that is not the actual policy of governments and may or may not ever become such, but a combination of effectively keeping the cooling radiative forcing while reducing the emissions causing warming would theoretically cause the greatest mitigation, if ever implemented.