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The Political Economy of Climate Change Science
The Political Economy of Climate Change Science

... operandum are exemplified by the dramatic shift in the opinion of WMO officials since 1975: “The cooling since 1940 has been large enough and consistent enough that it will not soon be reversed, and we are unlikely to quickly regain the ‘very extraordinary period of warmth’ that preceded it. Even th ...
Introduction to Climate change Study Cell
Introduction to Climate change Study Cell

... Arctic Sea Ice Prediction using community climate system model ...
Global Economy and Extreme Poverty
Global Economy and Extreme Poverty

... Due to change in salinity, if Artic keeps melting, this current could stop, creating a small ice age in Europe and North America. [IPCC] ...
Dual Impact Of Climate Change Intensifying vulnerability Achala Gupta
Dual Impact Of Climate Change Intensifying vulnerability Achala Gupta

Reinforced Theistic Manifest Destiny theory
Reinforced Theistic Manifest Destiny theory

... hunting, degrading environments, and introducing nonnative species). Still, many past effects pale compared to the threat of global climate change. (Nb. We will henceforth largely use the colloquial term, “global warming,” although of course not all locations may exhibit warming due to human-enhance ...
Introduction - San Jose State University
Introduction - San Jose State University

... http://www.ssec.wisc.edu/data/comp/cmoll/cmoll.html ...
Implications of the 1.5°C limit in the Paris
Implications of the 1.5°C limit in the Paris

... risks led many vulnerable countries to express concern that the former 2°C limit was too unsafe. These and other concerns led the world to adopt the Paris Agreement’s long-term temperature goal, which includes a 1.5°C limit, as opposed to the earlier 2°C goal adopted by the international communit ...
Source file - ICTP Portal
Source file - ICTP Portal

... “Patterns emerge that you wouldn’t recognize from just looking at either climatic or socioeconomic conditions,” said Diffenbaugh. For example, China has a relatively moderate expected climate change. However, when you combine that with the fact that it has the second largest economy in the world, a ...
PPT - cmmap
PPT - cmmap

... remove more than 4 GtC per year from the atmosphere • This free service provided by the planet constitutes an effective 50% emissions reduction, worth $400 Billion per year at today’s price on the ECX! • Science is currently unable to quantitatively account for ...
Changing Global Warming Beliefs with Scientific Information
Changing Global Warming Beliefs with Scientific Information

... hunting, degrading environments, and introducing nonnative species). Still, many past effects pale compared to the threat of global climate change. (Nb. We will henceforth largely use the colloquial term, “global warming,” although of course not all locations may exhibit warming due to human-enhance ...
Air Quality and Climate overview for teachers
Air Quality and Climate overview for teachers

... • Aerosol: Liquid or solid particles suspended in air • Wide range of chemical composition • Sizes range from <1nm to >10 μm ...
Impacts of Climate Change in the Pacific
Impacts of Climate Change in the Pacific

... sea waters of up to 80 per cent of the land mass in some areas. ...
Chapter 7 – global warming - Iowa State University Department of
Chapter 7 – global warming - Iowa State University Department of

Observed Strengthening of the Zonal Sea Surface Temperature Gradient
Observed Strengthening of the Zonal Sea Surface Temperature Gradient

Adriana G - Butler at UTB
Adriana G - Butler at UTB

Printer Friendly pdf
Printer Friendly pdf

... Even this overstates the effect of CO2, because the primary sources of these emissions—cars and power plants—also produce aerosols. Aerosols actually have a cooling effect on global temperatures, and the magnitude of this cooling approximately cancels out the warming effect of CO2.12 The surprising ...
Disappearing evidence
Disappearing evidence

... Paleoclimate Observing System (GPOS) to complement the recently established Global Climate, Terrestrial and Ocean Observing System (GCOS, GTOS, GOOS) that focus only on contemporary observations. There is no time to lose. Warming has been measured over most parts of the globe during the late 20th ce ...
The Impact of Global Warming on North Carolina
The Impact of Global Warming on North Carolina

... estate, insurance, and other economic sectors. Global warming are caused by environmental changes and weather processes. Global atmospheric circulation is influenced by seasonal variations of heat on earth. The Mountains and Piedmont generally experience lower temperatures while the Coast (Figure 2) ...
GEOENGINEERING: WORTHY OF CAUTIOUS EVALUATION? An
GEOENGINEERING: WORTHY OF CAUTIOUS EVALUATION? An

... material, but also because the relatively short lifetime of sulfate aerosols would necessitate multiple source regions to achieve roughly even coverage. Such coverage is likely important because the present experience with tropospheric aerosols is that they are concentrated regionally, and that at l ...
COM SEC(2007)
COM SEC(2007)

... decrease, mostly in Finland and the Baltic states: 25-50 fewer deaths per 100 000 persons each year.  Arctic region: Temperature increases are likely to be higher in the Arctic than anywhere else on Earth, resulting in accelerated melting of ocean and land ice and thawing of permafrost. In the Arct ...
Study of Impacts of Global Warming on Climate Change
Study of Impacts of Global Warming on Climate Change

... social, economic and ecological impacts), and large-scale high-impact events. ...
Avoiding Dangerous Climate Change - EEG, TU-Wien
Avoiding Dangerous Climate Change - EEG, TU-Wien

... The conference discussed the long-term implications of different levels of climate change for different sectors and for the world as a whole. Major themes included key vulnerabilities of the climate system and critical thresholds, socio-economic effects, both globally and regionally, emission pathwa ...
Observing climate change trends in ocean
Observing climate change trends in ocean

... • Analysis provides an estimate of timescales needed to distinguish climate change-driven trends from natural variability • Useful for assessing current datasets • Some datasets, some variables, have enough data to detect climate trend (if there is one) • But many don’t • Also useful for planning fu ...
Cool Bears + Warm Waters = Extinction?
Cool Bears + Warm Waters = Extinction?

Natural and forced air temperature variability in the Labrador region
Natural and forced air temperature variability in the Labrador region

... which suggests that models are currently unable to reproduce regional climate variability in Labrador air temperature. Using a combination of empirical statistical modeling and global climate models, we show that 33 % of the variability in annual Labrador air temperatures over the period 1881–2011 c ...
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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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