Not exact matches
Recent
regional scale analyses using satellite - based vegetation indices such as the Normalized
Difference Vegetation Index have found extensive areas of dryland greening
in areas of the Mediterranean, the Sahel, the Middle East and northern China, as well as greening
trends in Mongolia and South America, according to the paper.
Additionally, there were also
regional differences in the spatial patterns of change
trend in the ARNC temperature at a given time.
The result is that there is no
difference in regional cloud cover
trends, neither of precipitation, with increasing contamination and that the contaminated area has more dimming, but warmed more than the less contaminated area.
The reasons for the
regional differences in historical scaled - interannual and future 30 - year
trend regressions are unclear, since as noted above the model's interannual NAO variability does not appear to be affected by climate change between 1850 and 2045.
These
regional differences in amplitude notwithstanding, the large - scale features of the SLP, SAT and P regression maps show a strong degree of resemblance between the version based on historical scaled - interannual statistics and that based on future 30 - year
trends.
The results vary from region to region because of
differences in regional climate
trends as well as heating and cooling systems (for example, much of the northern part of the country relies on natural gas heating).
The only mention of RCS
in the Hantemirov's Thesis abstract is this sentence: To remove the age
trend, a method of
regional curves (Briffa et al., 1992), was used as which maintains the
differences between the growth rate of trees that existed
in various climatic epochs, i.e., allows to detect long - term fluctuations
in wood increases, exceeding the lifetime of individual trees.
What the annual evolution of the day to day max temp shows that this
difference is very small and does not have a
trend, and that min temps have rather large
regional drops then a recovery, And the daily
trend > N23 Lat of the change per day by year has evolved with a slight
trend in slope, but no
trend in offset.
As shown
in a previous large ensemble paper from those some authors (see figure 1
in that write - up), the global response across the ensemble is very similar even with those large
regional trend differences.
Such regionally varying effects may partly account for
differences between observed
regional global temperature
trends, and such effects must be understood to achieve accurate knowledge of how the climate dice are now loaded
in specific regions.
When we analyzed the limiting roles of temperature, soil moisture, and solar radiation independently, global average
trends masked
regional differences in the gains and losses of suitable plant growing days.