Chen, J., B.E. Carlson, and A.D. Del Genio, 2002: Evidence for strengthening of
the tropical general circulation in the 1990s.
The outflow temperature does not depend just on the local state but rather on conditions throughout the tropics, since
the tropical general circulation redistributes heat efficiently at high altitudes.
Chen, J., B.E. Carlson, and A.D. Del Genio, 2002: Evidence for strengthening of
the tropical general circulation in the 1990s.
Not exact matches
To simulate the
tropical climate to learn more about its processes, climate scientists have typically been relying on
general circulation models (GCMs) to simulate the
tropical climate.
Scientists at Pacific Northwest National Laboratory showed that global climate models are not accurately depicting the true depth and strength of
tropical clouds that have a strong hold on the
general circulation of atmospheric heat and the global water balance.
Mechoso, C.R., et al., 1995: The seasonal cycle over the
tropical Pacific in
general circulation model.
Hourdin, F., et al., 2006: The LMDZ4
general circulation model: Climate performance and sensitivity to parameterized physics with emphasis on
tropical convection.
The resulting wintertime cooling in the north Atlantic was rather severe, and the influences far from the north Atlantic included a
general southward shift of the
tropical circulations and drying of monsoonal and northern -
tropical regions where billions now live.
In Part I we outlined some
general features of the
tropical circulation, and discussed ways in which increases in anthropogenic greenhouse gases might affect El Niño.
Since the Eastern
Tropical Pacific is not entirely decoupled from West Wind Drift given the
general pattern of
circulation in the SE Pacific, the question arises is the magnitude of the observed overall energy difference in the recently observed «extended» La Nina phase of ENSO condition relative to the the «more normal» ENSO comparable in magnitude to energy associated with the apparent increase in winds and potentially currents around the Antarctic?
«The 21st - century intensification of dry seasons suggested by our analysis is probably partially driven by the
general intensification of
tropical circulation caused by increased temperatures and tropospheric moisture content.
Wong, S., and W. - C. Wang, 2003:
Tropical - extratropical connection in interannual variation of the tropopause: Comparison between NCEP / NCAR reanalysis and an atmospheric
general circulation model.
The
general circulation models assume that planetary cloud cover is either not affected by the CO2 forcing or assume planetary cloud cover is reduced by the CO2 forcing which explains why they have a
tropical tropospheric hot spot.
Sound waves, gravity waves, Rossby waves; numerical weather prediction; baroclinic instability;
general circulation;
tropical dynamics
Although previous studies have offered a
general global overview of water
circulation between the oceans and land, this traditional two - region model does not take into account the considerable precipitation that occurs over
tropical coastal regions, including the Indonesian maritime continent, the Indian subcontinent, and the Bay of Bengal.
This study evaluates the
tropical intraseasonal variability, especially the fidelity of Madden - Julian oscillation (MJO) simulations, in 14 coupled
general circulation models (GCMs) participating in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4).
«The authors write that «the notorious
tropical bias problem in climate simulations of global coupled
general circulation models manifests itself particularly strongly in the tropical Atlantic,»... they state that «the climate bias problem is still so severe that one of the most basic features of the equatorial Atlantic Ocean — the eastward shoaling thermocline — can not be reproduced by most of the IPCC assessment report models,... as they describe it, «show that the bias in the eastern equatorial Atlantic has a major effect on sea - surface temperature (SST) response to a rapid change in the Atlantic Meridional Overturning Circulation (AM
circulation models manifests itself particularly strongly in the
tropical Atlantic,»... they state that «the climate bias problem is still so severe that one of the most basic features of the equatorial Atlantic Ocean — the eastward shoaling thermocline — can not be reproduced by most of the IPCC assessment report models,... as they describe it, «show that the bias in the eastern equatorial Atlantic has a major effect on sea - surface temperature (SST) response to a rapid change in the Atlantic Meridional Overturning
Circulation (AM
Circulation (AMOC).»
A major enigma is that
general circulation climate models predict an immutable climate in response to decadal solar variability, whereas surface temperatures, cloud cover, drought, rainfall,
tropical cyclones, and forest fires show a definite correlation with solar activity.
The time - independent linear response to these
tropical anomalies is calculated for extratropical basic states taken from reanalysis climatologies and also from the climatological states of Action de Recherche Petite Echelle Grande Echelle (ARPEGE) and Laboratoire de Mà © tà © orologie Dynamique (LMDZ)
general circulation model simulations.
The major climate system indices that are operationally used at ICPAC include evolution of monsoons, medium and upper level winds, Madden - Julian Oscillation (MJO), Quasi Biennial Oscillation (QBO), El Niño Southern Oscillation, Indian Ocean dipole (IOD),
tropical cyclones, sea surface temperature gradients among many others that have been derived from
general circulation.
3) The
tropical tropospheric 8 km no hot spot Paradox (Strike 3 and the CAWG is disproved) The IPCC's
general circulation models predict that most amount of warming on the planet should occur in the tropics at 8k above the earth's surface.
Neelin, J. D., and and Coauthors,, 1992:
Tropical air — sea interaction in
general circulation models.
Mechoso, C. R., and and Coauthors,, 1995: The seasonal cycle over the
tropical Pacific in coupled ocean — atmosphere
general circulation models.
Tropical cyclones play an important role in the
general circulation of the atmosphere, accounting for 2 percent of the global annual rainfall and between 4 and 5 percent of the global rainfall in August and September at the height of the...
Charles, C.D., D. Rind, R. Healy, and R. Webb, 2001:
Tropical cooling and the isotopic composition of precipitation in
general circulation model simulations of the ice age climate.
Wang et al. (2012b) force the dynamical core of an atmospheric
general circulation model with warming in the
tropical troposphere that mimics the effects of climate change there.
The sensitivity of NPP to climate change is especially uncertain because it depends on changing soil water availability, which varies significantly between
General Circulation Models (GCMs), with some models suggesting major drying and reduced productivity in
tropical ecosystems (Cox et al., 2004).
Swann, A. L. S., Fung, I. Y. & Chiang, J. C. H. Mid-latitude afforestation shifts
general circulation and
tropical precipitation.
Xie (June 2008): The
Tropical Eastern Pacific Seasonal Cycle: Assessment of Errors and Mechanisms in IPCC AR4 Coupled Ocean — Atmosphere
General Circulation Models.
Effects of
tropical cyclones on ocean heat transport in a high resolution coupled
general circulation model.
The greater rate of warming in the
tropical mid-troposphere that is projected by
general -
circulation models is absent in this and all other observational datasets, whether satellite or radiosonde.
«Our results imply that because dust plays a role in modulating
tropical North Atlantic temperature, projections of these temperatures under various global warming scenarios by
general circulation models should account for long - term changes in dust loadings.