Those models will look at impacts such as
regional average temperature change, sea - level rise, ocean acidification, and the sustainability of soils and water as well as the impacts of invasive species on food production and human health.
Not exact matches
Determining the rate of
temperature change is more difficult at a local and
regional level because researchers have less data to
average, so trends are not as evident because of «statistical noise.»
Even if global warming is limited to these levels,
changes in
regional temperatures (and therefore climate
change impacts) can vary significantly from the global
average.
Human induced trend has two components, namely (a) greenhouse effect [this includes global and local /
regional component] and (b) non-greenhouse effect [local /
regional component]-- according to IPCC (a) is more than half of global
average temperature anomaly wherein it also includes component of volcanic activities, etc that comes under greenhouse effect; and (b) contribution is less than half — ecological
changes component but this is biased positive side by urban - heat - island effect component as the met network are concentrated in urban areas and rural - cold - island effect is biased negative side as the met stations are sparsely distributed though rural area is more than double to urban area.
While the anomalous nature of recent trends in global
average temperature is often highlighted in discussions of climate
change,
changes at
regional scales have potentially greater societal significance.
High - frequency associations (not shown here) remain strong throughout the whole record, but
average density levels have continuously fallen while
temperatures in recent decades have risen... As yet, the reason is not known, but analyses of time - dependent
regional comparisons suggest that it is associated with a tendency towards loss of «spring» growth response (Briffa et al., 1 999b) and, at least for subarctic Siberia, it may be connected with
changes in the timing of spring snowmelt (Vaganov et al., 1999).
Even though the
average temperature stayed the same, there were still
regional changes, with cooling in the tropics and warming at both poles (particularly in their respective winters):
But the current rise in Arctic
temperature is due not to
changes in global
average temperature but to
changes in
regional weather patterns.
They clearly have not «proved» skill at predicting in a hindcast mode,
changes in climate statistics on the
regional scale, and even in terms of the global
average surface
temperature trend, in recent years they have overstated the positive trend.
Changes in instrumentation and data availability have caused time - varying biases in estimates of global - and
regional -
average sea - surface
temperature.
Rohde, R. et al: «A new estimate of the
average earth surface land
temperature spanning 1753 to 2011», Manuscript: text presented at the 3rd Santa Fe conference on global and
regional climate
temperature change, 2011
As in the allegory, a «global
average»
temperature obscures critical dynamics that are best understood by examining local causes of «
regional climate»
change.
Other factors, including greenhouse gases, also contributed to the warming and
regional factors played a significant role in increasing
temperatures in some regions, most notably
changes in ocean currents which led to warmer - than -
average sea
temperatures in the North Atlantic.
Adding data from around the world, however, indicates that the Medieval Warm Period was mainly a
regional phenomenon, with warming in one region offsetting cooling in other regions, leaving little
change in the
average global
temperature.
Note that
regional proxies, such as the oxygen - isotope
temperature reconstructions from the Greenland Ice Core Project that record Dansgaard - Oeschger events, often indicate faster
regional rates of climate
change than the overall global
average for glacial - interglacial transitions, just as today warming is more pronounced in Arctic regions than in equatorial regions (Barnosky et al., 2003; Diffenbaugh and Field, 2013).
In other words,
regional temperatures change, but the
average global
temperature doesn't.
Recent meta - analyses indicate that on
average, examined terrestrial species have been moving poleward about 1.76 km / yr (reported as 17.6 + 2.9 km / decade), apparently keeping pace with
regional temperature change, although species range shifts to higher elevations have on
average lagged behind climate (Chen et al., 2011).
The impact on global
average temperature seems indeed to be small; however,
changing the flow of energy produces large
regional impacts».
These range from simple
averaging of
regional data and scaling of the resulting series so that its mean and standard deviation match those of the observed record over some period of overlap (Jones et al., 1998; Crowley and Lowery, 2000), to complex climate field reconstruction, where large - scale modes of spatial climate variability are linked to patterns of variability in the proxy network via a multivariate transfer function that explicitly provides estimates of the spatio - temporal
changes in past
temperatures, and from which large - scale
average temperature changes are derived by
averaging the climate estimates across the required region (Mann et al., 1998; Rutherford et al., 2003, 2005).
Although there might be «slowdowns and accelerations in warming lasting a decade or more,» they write, the clear long - term trend is «substantial increases in global
average surface
temperature and important
changes in
regional climate.»
Using existing output data from global climate models, the researchers plotted projections of
changes in global
average temperature and rainfall against
regional changes in daily extremes.