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Where Are You From? Why Are You Here? An African Perspective
Where Are You From? Why Are You Here? An African Perspective

... and similarities among the three tropical oceans. The winds that force the Atlantic and Pacific are similar, but those ocean basins respond differently because one is three times as wide as the other. The Atlantic and Indian oceans have similar dimensions, but smoothly varying trade winds prevail ove ...
Reconsidering the Climate Change Act
Reconsidering the Climate Change Act

... Society to the resignation letter of the late Hal Lewis (a distinguished physicist and a fellow of the Society): On the matter of global climate change, APS notes that virtually all reputable scientists agree with the following observations: Carbon dioxide is increasing in the atmosphere due to huma ...
- Wiley Online Library
- Wiley Online Library

... yellowfin (Thunnus albacares), and bigeye (Thunnus obesus), as well as other species (FAO, 2012). Tunas occupy specific thermal habitats at different life stages and have a high metabolic demand (Lehodey et al., 2011, 2013). Thus, changes to either thermal habitat or ocean productivity are likely to ...
'Sensitivity of climate change detection and attribution to the characterization of internal climate variability'
'Sensitivity of climate change detection and attribution to the characterization of internal climate variability'

... climate system that would occur in the absence of natural or anthropogenic forcings, solely ...
What to Do? Does Science have a Role?
What to Do? Does Science have a Role?

... • But to be effective a Climate Policy Panel will need to develop a new suite of Integrated Assessment (coupled climate-socioeconomic) models ...
Relative climatic effects of landcover change and
Relative climatic effects of landcover change and

Predicting species distribution of Sierra Nevada butterflies in
Predicting species distribution of Sierra Nevada butterflies in

... (Garmin eTrex Vista) was used to determine the locality of all collections within <20m error. Modeling: Models were made using BIOCLIM and MAXENT. BIOCLIM (Nix, 1986) is a commonly used modeling program which relates climatic parameters (i.e. temperature, precipitation, moisture, etc.) to species pr ...
Please click on this link
Please click on this link

... Beyond the mean warming, climate change may modify the temperature variability, with consequences on extreme events causing societal and environmental impacts. Here we focus on European summer temperatures and assess future changes in both the intra-seasonal variability and extreme events (heat wave ...
Vol.12, No. 2
Vol.12, No. 2

... mum wind speed is to increase (Figure 3) by 6.6% in the North Indian Ocean to 10% in the North Atlantic. Formation Region. The model projects several shifts in the formation region of tropical cyclones. In the Northern Hemisphere, the formation regions tend to shift to higher latitudes: in the North ...
22. Predictions and Projections of Pine Productivity and Hydrology
22. Predictions and Projections of Pine Productivity and Hydrology

Using Biogeochemical Process Models to Quantify Greenhouse Gas
Using Biogeochemical Process Models to Quantify Greenhouse Gas

... While we have a rough but relatively clear picture as to where some of the biggest opportunities lie for changing agricultural practices to achieve greater efficiencies and mitigate GHGs (Smith et al. 2008), we have less clarity on how to quantify such changes at local scales. The Intergovernmental ...
1 The Effects of Artificial Clouds on Climate
1 The Effects of Artificial Clouds on Climate

... G. Water vapor introduced by jets into the lower stratosphere also destroys the ozone layer, which could affect the levels of solar radiation reaching the ground. 17 H. Cloud-seeding flares use toxic chemicals, including silver iodide, aluminum, strontium and magnesium. These chemicals and have been ...
Powerpoint - Oceanclimate.de
Powerpoint - Oceanclimate.de

... Everything is maintained through water. Ocean; give us your enternal power. J.W. v. Goethe (11749-1832) , Drama - Faust II ...
Silva2013-ERL-APMortality.pdf
Silva2013-ERL-APMortality.pdf

... modeled concentrations from an ensemble of chemistry–climate models to estimate the global burden of anthropogenic outdoor air pollution on present-day premature human mortality, and the component of that burden attributable to past climate change. Using simulated concentrations for 2000 and 1850 an ...
Vol.10, No.2, 2010
Vol.10, No.2, 2010

Global premature mortality due to anthropogenic outdoor air pollution and... past climate change
Global premature mortality due to anthropogenic outdoor air pollution and... past climate change

... modeled concentrations from an ensemble of chemistry–climate models to estimate the global burden of anthropogenic outdoor air pollution on present-day premature human mortality, and the component of that burden attributable to past climate change. Using simulated concentrations for 2000 and 1850 an ...
Consistency analysis
Consistency analysis

Internally and Externally Caused Climate Change
Internally and Externally Caused Climate Change

... A numerical climate model is used to simulate climate change forced only by random fluctuations of the atmospheric heat transport. This short-term natural variability of the atmosphere is shown to be a possible "cause" not only of the variability of the annual world average temperature about its mea ...
RT4: Understanding the processes governing climate variability and
RT4: Understanding the processes governing climate variability and

... RT4: Aim (1) The uncertainty about climate sensitivity has not decreased between SAR (1995) and TAR (2001) of IPCC. - How does that affect an approach based on ENSEMBLES of model simulations? ...
Quick overview of the activities in this module
Quick overview of the activities in this module

... these module instructions will need to be periodically updated to account for changes in the code. If you find any errors, please contact the module developers. Visit our website: github.com/GRAPLE/GRAPLEr/wiki for the most recent version of the R packages for this module. Why this matters: Lakes ar ...
Written Testimony for the House Committee on Science, Space, and... Hearing on “Examining the UN Intergovernmental Panel on Climate Change...
Written Testimony for the House Committee on Science, Space, and... Hearing on “Examining the UN Intergovernmental Panel on Climate Change...

Sounding Paper for METR 3613 - University of Oklahoma School of
Sounding Paper for METR 3613 - University of Oklahoma School of

... Conclusions and Summary As the day progressed, the boundary layer increased in depth due to surface heating (thermal eddies) and weak turbulence, with the largest increase in depth occurring between 1400 UTC and 1700 UTC. This boundary layer depth increase was marked by an increase in height of the ...
Talk 1
Talk 1

... there is a vertical dimension because atmospheric processes change as you move vertical above the Earth’s surface. ...
Earth system sensitivity inferred from Pliocene modelling and data
Earth system sensitivity inferred from Pliocene modelling and data

... Where the proxy data are most abundant, in the Quaternary period, atmospheric CO2 concentrations were never significantly higher than pre-industrial17 , reducing the relevance of this period for future climate change considerations. However, a combined palaeoclimate modelling and data approach can b ...
Co-chairs (2)
Co-chairs (2)

... a: These estimates are assessed from a hierarchy of models that encompass a simple climate model, several Earth System Models of Intermediate Complexity and a large number of Atmosphere-Ocean General Circulation Models (AOGCMs). b: Year 2000 constant composition is derived from AOGCMs only. ...
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Atmospheric model



An atmospheric model is a mathematical model constructed around the full set of primitive dynamical equations which govern atmospheric motions. It can supplement these equations with parameterizations for turbulent diffusion, radiation, moist processes (clouds and precipitation), heat exchange, soil, vegetation, surface water, the kinematic effects of terrain, and convection. Most atmospheric models are numerical, i.e. they discretize equations of motion. They can predict microscale phenomena such as tornadoes and boundary layer eddies, sub-microscale turbulent flow over buildings, as well as synoptic and global flows. The horizontal domain of a model is either global, covering the entire Earth, or regional (limited-area), covering only part of the Earth. The different types of models run are thermotropic, barotropic, hydrostatic, and nonhydrostatic. Some of the model types make assumptions about the atmosphere which lengthens the time steps used and increases computational speed.Forecasts are computed using mathematical equations for the physics and dynamics of the atmosphere. These equations are nonlinear and are impossible to solve exactly. Therefore, numerical methods obtain approximate solutions. Different models use different solution methods. Global models often use spectral methods for the horizontal dimensions and finite-difference methods for the vertical dimension, while regional models usually use finite-difference methods in all three dimensions. For specific locations, model output statistics use climate information, output from numerical weather prediction, and current surface weather observations to develop statistical relationships which account for model bias and resolution issues.
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