Climate -
related ecosystem effects are also already evident in the mid-latitudes, such as on the island of Hokkaido, Japan, where a decrease in alpine flora has been reported (Kudo et al., 2004).
Much of the inter-annual to decadal scale variability in surface air temperature (SAT) anomaly patterns and
related ecosystem effects in the Arctic and elsewhere can be attributed to the superposition of leading modes of variability in the atmospheric circulation.
Not exact matches
But the fact of the influence of anthropogenic CO2 on the climate is distinct to facts of the degree of that
effect, which is again logically distinct from the facts
relating to the
effects produced as second, third, and fourth order
effects on climate systems,
ecosystems, species, primary industry and civil infrastructure, economy, and society.
The observed
effects of cryosphere reduction include modification of river regimes due to enhanced glacial melt, snowmelt advance and enhanced winter base flow; formation of thermokarst terrain and disappearance of surface lakes in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven by ice and permafrost melting; regional ocean freshening; sea - level rise due to glacier and ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine
ecosystems affected by lake - ice and sea - ice reduction; changes in livelihoods; reduced tourism activities
related to skiing, ice climbing and scenic activities in cryospheric areas affected by degradation; and increased ease of ship transportation in the Arctic.
We're also seeing similarly dramatic changes in other aspects of climate and
related effects on
ecosystems, including the distribution of rainfall, storm activity, extinction of plant and animal species, and seasonal change.