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Prediction of Future Change of Water Demand Following Global
Prediction of Future Change of Water Demand Following Global

... all the models. Since temperature rise for MRI is less than other two models, higher yields are expected to occur. However, biomass of more than 23 ton/ha may be too high. The reason why grain yield for all the models increases can not be explained well. In case of maize, both biomass and grain yiel ...
Exploring the relationship between climate change and rice yield in
Exploring the relationship between climate change and rice yield in

... where YBoro is the yield of Boro rice (in kg per acre), max t is the average maximum temperature (°C) from December to May, min t is the average minimum temperature (°C) from December to May, train is the total rainfall (mm) from December to May, et is the error term, and t is the time (i.e., year). ...
Climate change implications for fisheries and aquaculture
Climate change implications for fisheries and aquaculture

... El Niño (e.g. 1997–1998) and El Niña (e.g. 2011) events. The satellite altimetry method, available since 1993, has provided evidence that the sea level in the warm pool of the western Pacific is increasing at rates three times higher than the GMSL, while rates for most parts of the eastern Pacific a ...
With Speed and Violence Fred Pearce
With Speed and Violence Fred Pearce

... below. That water will not return to the surface for a thousand years. The chimney, once one of a family, pursues its lonely task in the middle of one of the coldest and most remote seas on Earth. And its swirling waters may be the switch that can turn the heat engine of the world's climate system o ...
Sensitivity and response of northern hemisphere altitudinal and
Sensitivity and response of northern hemisphere altitudinal and

... history, including climatic changes, wildfires, human impact, insect infestations and plant diseases play a very important role and have to be considered at the landscape scale when discussing sensitivity of the so-called climatic treeline to changing climate. Heat deficiency is a very complex facto ...
Antarctic Stratification, Atmospheric Water Vapor, and Heinrich Events
Antarctic Stratification, Atmospheric Water Vapor, and Heinrich Events

Soil drying in Europe and its impact on atmospheric
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Climate Change: An Overview and its Impact on the Living Lakes
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AIACC Regional Study Abstracts
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DANGER The of Corporate Landfill Gas-to-Energy Schemes and How to Fix It
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Changes in alpine plant growth under future climate conditions
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The Effects of Climate Change on the Full Enjoyment of Human Rights
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national sweater day - WWF
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Development of a Methodology and a Tool for the Assessment of Vulnerability of Roadways to Flood Induced Damage
Development of a Methodology and a Tool for the Assessment of Vulnerability of Roadways to Flood Induced Damage

... model can capture it. Another key aspect of the system dynamics approach is the ability to show the root cause (or causes) of a problem. This is because a good system dynamics model can include all of the essential elements and their interdependencies and hence, the relational dynamics. The steps in ...
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Global change and eutrophication of coastal waters

... gases and rising temperatures. The effects of global climate change (GCC) are already detectable in the decline in snow cover, glaciers and polar ice, which have led to a poleward shift in plant and animal distributions, and caused changes in algal and fish communities and foodwebs (IPCC, 2007). The ...
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... important for transportation planners and analysts in the future. It may be that Pisarski’s work will be too difficult to replicate in the future without the census long form. Pisarski also identifies trends that should be followed in the future: immigration, suburban commuting, telecommuting. He ca ...
Estimates of the Damage Costs of Climate Change
Estimates of the Damage Costs of Climate Change

... the issue of consistency, say, between sea level impact in Europe and Japan, is left to the specialist. Impact categories where such sources are unavailable are not included. As an additional selection criterion, only sources are used that are based on climate scenarios from GCMs. This study is the ...
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... politics. It’s what one politician uses to convince another politician to support a particular piece of legislation. Some would call it “one hand washing the other” and that’s a fair analogy. For the President to advance a political agenda, political capital is his fuel tank to get things done. He w ...
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WHY ADVOCATE ON CLIMATE CHANGE?

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Nonlinear response of mid-latitude weather to the changing Arctic
Nonlinear response of mid-latitude weather to the changing Arctic

... of this influence relative to non-Arctic factors, and is it limited to specific regions, seasons, or ...
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Strategy for FAO’s work on climate change – roadmap

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Climate Change and Public Health 101

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Tracking Climate Change Opinions from Twitter Data Xiaoran An Auroop R. Ganguly
Tracking Climate Change Opinions from Twitter Data Xiaoran An Auroop R. Ganguly

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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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