For example, while
significant changes in the vegetation or built environment surrounding a weather station may not be included in historical metadata, they may cause significant changes in the exposure of the instruments.
Not exact matches
Studies including Wang's earlier work
in Africa have shown that even small
changes in soil moisture
in drylands could be
significant enough to cause large
changes in vegetation productivity.
So if you think of going
in [a] warming direction of 2 degrees C compared to a cooling direction of 5 degrees C, one can say that we might be
changing the Earth, you know, like 40 percent of the kind of
change that went on between the Ice Age; and now are going back
in time and so a 2 - degree
change, which is about 4 degrees F on a global average, is going to be very
significant in terms of
change in the distribution of
vegetation,
change in the kind of climate zones
in certain areas, wind patterns can
change, so where rainfall happens is going to shift.
Besides the increased emissions of N2O, the authors observed
significant increases
in the seasonal release of CO2 and CH4 as a result of only a mild temperature increase, and dug deeply into the reason behind the observed
changes by detailed soil and
vegetation measurements.
With respect to why there was a
significant increase
in tree density over the past several decades, Dolanc offers that the
changes in the density and composition of lower - elevation forests are consistent with fire suppression; but that the density increases
in high - elevation
vegetation types (subalpine forests generally don't burn) are «more likely to be caused by
changing climate.»
A
significant component of this key ecosystem characteristic is dependent on relatively slow processes such as rates of recuitment, mortality, and
changes in vegetation composition.
These moist enthalpy - related studies confirm previous results showing that
changes in vegetation cover, surface moisture and energy fluxes generally lead to
significant climatic
changes (e.g. 41 - 43) and responses which can be of a similar magnitude to that projected for future greenhouse gas concentrations (44, 45).