Not exact matches
«This emphasizes the importance of large - scale energy transport and
atmospheric circulation changes in restoring Earth's global temperature equilibrium after a
natural, unforced warming event,» Li said.
Your statement that «Thus it is
natural to look at the real world and see whether there is evidence that it behaves
in the same way (and it appears to, since model hindcasts of past
changes match observations very well)» seems to indicate that you think there will be no
changes in ocean
circulation or land use trends, nor any subsequent
changes in cloud responses thereto or other
atmospheric circulation.
As discussed
in the Climate chapter, large - scale
atmospheric circulation patterns connected to
changes in sea - surface temperatures strongly influence
natural variations
in precipitation and temperature (e.g., Cayan et al. 1999; Mantua and Hare 2002).
Natural factors contributing to past climate
change are well documented and include
changes in atmospheric chemistry, ocean
circulation patterns, solar radiation intensity, snow and ice cover, Earth's orbital cycle around the sun, continental position, and volcanic eruptions.
«It's important to determine where we believe that some of the recent trends
in circulation could potentially be linked with climate
change, rather than just
natural variability,» Ted Shepherd, an
atmospheric scientist at the University of Reading
in the U.K., said
in an email.
Included
in resource are the following topics:
Natural causes of climate
change Evidence of climate
change Global Warming Causes and effects of climate
change Global
atmospheric circulation Tropical storms causes, characteristics, location and frequency Causes of EL Nino Effects of the Big Dry Adaptation to drought At the end of the resources are pupil booklets.
Global
changes of the
atmospheric composition and
natural circulation changes are
in competition to each other
in determining the Arctic surface climate.
Your statement that «Thus it is
natural to look at the real world and see whether there is evidence that it behaves
in the same way (and it appears to, since model hindcasts of past
changes match observations very well)» seems to indicate that you think there will be no
changes in ocean
circulation or land use trends, nor any subsequent
changes in cloud responses thereto or other
atmospheric circulation.
Energy budgets
change all the time from large
natural variations
in ocean and
atmospheric circulation.
On the other hand, satellite - observed
changes in absorbed sunlight and emitted heat
in the tropics over the period 1985 - 2000, which appear to have caused a strengthening of the tropical
atmospheric circulation, could
in principle be either anthropogenic or
natural in origin.
LONDON, 17 March, 2017 — Scientists have calculated that at least 30 % and perhaps one half of the decline
in Arctic summer sea ice could be attributed to
natural causes —
changes of ocean and
atmospheric circulation that happen according to some long - term cycle.
These aspects of precipitation generally exhibit large
natural variability, and El Niño and
changes in atmospheric circulation patterns such as the North Atlantic Oscillation have a substantial influence.
In both the tropics and extratropics, it is difficult to discern significant long - term trends in the patterns of climate variability from natural variability, never mind abrupt (threshold) changes in the atmospheric circulatio
In both the tropics and extratropics, it is difficult to discern significant long - term trends
in the patterns of climate variability from natural variability, never mind abrupt (threshold) changes in the atmospheric circulatio
in the patterns of climate variability from
natural variability, never mind abrupt (threshold)
changes in the atmospheric circulatio
in the
atmospheric circulation.
In addition, human - induced climate
change may alter
atmospheric circulation, dislocating historical patterns of
natural variability and storminess.
These climate
changes are a result of human and
natural climate forcings and feedbacks — the relative role of each
in altering
atmospheric and ocean
circulation features, and even the global annual average radiative forcing, however, is still uncertain.