Not exact matches
Resulting
changes in the atmospheric temperature structure, including from surface dimming,
in turn affect
regional circulation and precipitation patterns.
The top priorities should be reducing uncertainties
in climate sensitivity, getting a better understanding of the effect of climate
change on atmospheric
circulation (critical for understanding of
regional climate
change,
changes in extremes) and reducing uncertainties
in radiative forcing — particularly those associated with aerosols.
The climate
change in this period is generally believed to be associated with precessional
changes in the distribution of solar radiation, which primarily affect land - sea temperature contrast, and give only a
regional warming, plus an enhancement of certain monsoonal
circulations.
Various mechanisms, involving
changes in ocean
circulation,
changes in atmospheric concentrations of greenhouse gases or haze particles, and
changes in snow and ice cover, have been invoked to explain these sudden
regional and global transitions.
Current state - of - the - art general
circulation models have difficulty simulating the
regional distribution of monsoon rainfall, the 24 June review
in Nature Climate
Change says.
Yet, we explained there is also reasonable basis for concern that a warming world may at least temporarily increase tornado damage including the fact that oceans are now warmer, and
regional ocean
circulation cycles such as La Nina / El Nino patterns
in the Pacific which affect upper atmospheric conditions appear to becoming more chaotic under the influence of climate
change.
By Amber Bentley (Aged 11)
In just 16 pages, this wonderful book covers the structure of the atmosphere, solar radiation, the water cycle, clouds, fronts, convection, air pressure, air masses, the global atmospheric
circulation, making weather observations, forecasting, synoptic charts, hurricanes,
regional climate, palaeoclimates and anthropogenic climate
change.
Current global multi-decadal predictions are unable to skillfully simulate
regional forcing by major atmospheric
circulation features such as from El Niño and La Niña and the South Asian monsoon, much less
changes in the statistics of these climate features.
The assumption of a global annual average increase
in the coming decades +1 C and +2 C, is of little use
in defining
changes in climate impacts at the
regional and local scale, which are so dependent
in how large scale
circulation features would
change in the coming decades.
These results suggest that both global and
regional climate models may fail to translate projected
circulation changes into their likely rainfall impacts
in southeast Australia.
«The authors write that North Pacific Decadal Variability (NPDV) «is a key component
in predictability studies of both
regional and global climate
change,»... they emphasize that given the links between both the PDO and the NPGO with global climate, the accurate characterization and the degree of predictability of these two modes
in coupled climate models is an important «open question
in climate dynamics» that needs to be addressed... report that model - derived «temporal and spatial statistics of the North Pacific Ocean modes exhibit significant discrepancies from observations
in their twentieth - century climate... conclude that «for implications on future climate
change, the coupled climate models show no consensus on projected future
changes in frequency of either the first or second leading pattern of North Pacific SST anomalies,» and they say that «the lack of a consensus
in changes in either mode also affects confidence
in projected
changes in the overlying atmospheric
circulation.»»
Such
circulation changes are the main cause of variations
in climate elements on a
regional scale, sometimes mediated by parallel
changes in the land surface (IPCC, 1990, 1996).
This section documents
regional changes and slow fluctuations
in atmospheric
circulation over past decades, and demonstrates that these are consistent with large - scale
changes in other variables, especially temperature and precipitation.
«Greenland ice takes on a new role
in the climate
change story, not just indicating
change and contributing to sea level rise, but possibly playing an important role
in destabilizing
regional if not global ocean
circulation that naturally exchanges heat north - south,» said Jason Box of the Geological Survey of Denmark and Greenland, and a study co-author,
in an email to Mashable.
Scientists have recently observed major
changes in these glaciers: several have broken up at the ocean end (the terminus), and many have doubled the speed at which they are retreating.2, 5 This has meant a major increase
in the amount of ice and water they discharge into the ocean, contributing to sea - level rise, which threatens low - lying populations.2, 3,5 Accelerated melting also adds freshwater to the oceans, altering ecosystems and
changing ocean
circulation and
regional weather patterns.7 (See Greenland ice sheet hotspot for more information.)
Shows that the
changes in discharge extremes are related to the
regional pluriannual rainfall variability and the associated atmospheric
circulation as well as to tropical large - scale climatic indicators
However, there are no compelling data to suggest a confluence of climate -
change impacts that would affect global production
in either direction, particularly because relevant fish population processes take place at
regional or smaller scales for which general
circulation models (GCMs) are insufficiently reliable.
Climate
change was assessed by means of two Long Ashton Research Station - Weather Generator (LARS - WG) weather generators and all outputs from the available general circulation models in the Model for the Assessment of Greenhouse - gas Induced Climate Change - SCENario GENerator (MAGICC - SCENGEN) software, in combination with different emission scenarios at the regional scale, while the Providing Regional Climates for Impacts Studies (PRECIS) model has been used for projections at the local
change was assessed by means of two Long Ashton Research Station - Weather Generator (LARS - WG) weather generators and all outputs from the available general
circulation models
in the Model for the Assessment of Greenhouse - gas Induced Climate
Change - SCENario GENerator (MAGICC - SCENGEN) software, in combination with different emission scenarios at the regional scale, while the Providing Regional Climates for Impacts Studies (PRECIS) model has been used for projections at the local
Change - SCENario GENerator (MAGICC - SCENGEN) software,
in combination with different emission scenarios at the
regional scale, while the Providing
Regional Climates for Impacts Studies (PRECIS) model has been used for projections at the local scale.
We should be able to predict
changes in global temperature trends from the net latitudinal position of all the air
circulation systems and
regional climate
changes follow from those latitudinal shifts.
xii) All
regional climate
changes are a result of movement
in relation to the locally dominant air
circulation systems which move cyclically poleward and equatorward.
Future climate
change may cause either an increase or a decrease
in background tropospheric ozone, due to the competing effects of higher water vapour and higher stratospheric input; increases
in regional ozone pollution are expected due to higher temperatures and weaker
circulation.
First, Baines and Folland pulled together a range of
regional changes in temperature, rainfall, and atmospheric
circulation around the Atlantic that could all be tied back to a cooling of the North Atlantic.
US CLIVAR is engaging with the SEARCH Program to define common research topics, including
changes in climate, sea ice extent, ice sheet mass
in the Arctic basin, and climate impacts on ocean
circulation and
regional sea level.