Not exact matches
January 2004: «Directions for Climate Research» Here, ExxonMobil outlines areas where it deemed more research was necessary, such as «natural climate variability, ocean currents and heat transfer, the
hydrological cycle, and the ability of climate models to predict
changes on a
regional and local scale.»
These
changes made China a unique region to investigate the impact of aerosols on
regional climate and the
hydrological cycle.
The findings represent evidence for considerable
changes in
regional hydrological cycles following greenhouse gas emissions.
Using this approach, we prove that
changes in climatic and
hydrological parameters at global and
regional scales are directly or indirectly reflected in sea - level regime.
Contribution from working group I to the fifth assessment report by IPCC TS.5.4.1 Projected Near - term
Changes in Climate Projections of near - term climate show small sensitivity to Green House Gas scenarios compared to model spread, but substantial sensitivity to uncertainties in aerosol emissions, especially on
regional scales and for
hydrological cycle variables.
The Swedish Meteorological and
Hydrological Institute (SMHI) presents unique data which depict
regional climate
change after a rise in global temperature of 1.5 degrees.
These stationary - wave
changes lead to large
regional changes in the
hydrological cycle and modify the sensitivity of the
hydrological cycle to global warming.
Methodological advances since the TAR have focused on exploring the effects of different ways of downscaling from the climate model scale to the catchment scale (e.g., Wood et al., 2004), the use of
regional climate models to create scenarios or drive
hydrological models (e.g., Arnell et al., 2003; Shabalova et al., 2003; Andreasson et al., 2004; Meleshko et al., 2004; Payne et al., 2004; Kay et al., 2006b; Fowler et al., 2007; Graham et al., 2007a, b; Prudhomme and Davies, 2007), ways of applying scenarios to observed climate data (Drogue et al., 2004), and the effect of
hydrological model uncertainty on estimated impacts of climate
change (Arnell, 2005).
Constraining the response of the
hydrological cycle, land surface and
regional weather to global climate
change.
Variations in
regional hydrological processes and water resources and their response to
change in the environment such as the increase of greenhouse gases will be examined.
But as Media Matters for America noted when Stossel previously downplayed the threat posed by global warming, the Intergovernmental Panel on Climate
Change (IPCC) concluded in 2001 that» [r] ecent
regional changes in climate, particularly increases in temperature, have already affected
hydrological systems and terrestrial and marine ecosystems in many parts of the world.»
Paper: Reference: Yun Qian, William I. Gustafson Jr., L. Ruby Leung, Steven J. Ghan, Effects of soot - induced snow albedo
change on snowpack and
hydrological cycle in western U.S. based on WRF chemistry and
regional climate simulations, Journal of Geophysical Research - Atmospheres, 2009, doi: 10.1029 / 2008JD011039