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Top margin 1
Top margin 1

... Climate change and the EU’s response What is the problem? The world is getting rapidly warmer, and there is an overwhelming consensus among the leading climate scientists that this is being caused mainly by carbon dioxide and other 'greenhouse gases' emitted by human activities, chiefly the combusti ...
Evolutionary and plastic responses of freshwater invertebrates to
Evolutionary and plastic responses of freshwater invertebrates to

... 2012). We therefore will start with an overview of what is known with regard to responses of freshwater invertebrates to the latter two conditions. The major part of the present synthesis will, however, deal with the effects of temperature as these have been studied in more detail and explicitly in ...
Effects of 20th Century Climate Change on Mountain Watersheds in
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... • Transient SWE simulation from HadCM3 (A2) GCM run (with running 10 year average smoothing) • Simulated from observed climate shows a declining trend of ~3KAF per decade (19352000) • HadCM3 simulated declines ~4KAF per decade Figure courtesy of Matt Wiley and Richard Palmer at CEE, UW ...
CO2 as a primary driver of Phanerozoic climate: COMMENT
CO2 as a primary driver of Phanerozoic climate: COMMENT

... Royer et al. do not dispute the existence of the CRF/temperature correlation of Shaviv and Veizer (2003), only its role relative to that of CO2. The CRF effect should therefore be incorporated as a complementary factor into the existing climate models. Once this solar amplification is included, the ...
global climate change
global climate change

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Forecasting global climate change: A scientific approach Kesten C
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Global Warming and Climate Change
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Climate Change and the Water Cycle
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Russia and Neighbouring Countries: Environmental, Economic and
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Defeating Kyoto: The Conservative Movement`s Impact on U.S.
Defeating Kyoto: The Conservative Movement`s Impact on U.S.

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Contributions to the management of Chancay
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Defeating Kyoto: The Conservative Movement`s Impact
Defeating Kyoto: The Conservative Movement`s Impact

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scvwd_system_climate_analysis_v0.01

... 2013; Ficklin et al., 2012) and around the globe (Girvetz et al., 2009) in studies of the hydrological impact of climate change. As part of a past effort (Reclamation, 2011), the downscaled precipitation and temperature projections for the period 1950-2099 were used to drive the Variable Infiltratio ...
Effect of Green House Gases and Human Population in Global
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... When this experiment is set-up according to the prescription on the NOAA webpage, it is quite possible to get a difference of temperature of 10C between or among ...
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Climate__Vector___Di.. - Erasmus Mundus Students and Alumni

... Malaysia Meteorological Department http://www.met.gov.my Ministry of Health http://www.moh.gov.my/MohPortal/ Hassan, Kumar & Kumarenthiran, 2008, “Climate Change Scenario and the Impact of Global Warming on the Winter Monsoon”, paper presented at the Second National Conference on Extreme Weather and ...
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Global warming hiatus



A global warming hiatus, also sometimes referred to as a global warming pause or a global warming slowdown, is a period of relatively little change in globally averaged surface temperatures. In the current episode of global warming many such periods are evident in the surface temperature record, along with robust evidence of the long term warming trend.The exceptionally warm El Niño year of 1998 was an outlier from the continuing temperature trend, and so gave the appearance of a hiatus: by January 2006 assertions had been made that this showed that global warming had stopped. A 2009 study showed that decades without warming were not exceptional, and in 2011 a study showed that if allowances were made for known variability, the rising temperature trend continued unabated. There was increased public interest in 2013 in the run-up to publication of the IPCC Fifth Assessment Report, and despite concerns that a 15-year period was too short to determine a meaningful trend, the IPCC included a section on a hiatus, which it defined as a much smaller increasing linear trend over the 15 years from 1998 to 2012, than over the 60 years from 1951 to 2012. Various studies examined possible causes of the short term slowdown. Even though the overall climate system had continued to accumulate energy due to Earth's positive energy budget, the available temperature readings at the earth's surface indicated slower rates of increase in surface warming than in the prior decade. Since measurements at the top of the atmosphere show that Earth is receiving more energy than it is radiating back into space, the retained energy should be producing warming in at least one of the five parts of Earth's climate system.A July 2015 paper on the updated NOAA dataset cast doubt on the existence of this supposed hiatus, and found no indication of a slowdown. This analysis incorporated the latest corrections for known biases in ocean temperature measurements, and new land temperature data. Scientists working on other datasets welcomed this study, though the view was expressed that the short term warming trend had been slower than in previous periods of the same length.
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