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draft decision - Meetings
draft decision - Meetings

... Parties should strengthen their cooperation on enhancing action on adaptation, taking into account the Cancun Adaptation Framework, particularly item (c) paragraph 7 of Article 7, “Strengthening scientific knowledge on climate, including research, systematic observation of the climate system and ear ...
Climate, Ecology, and Human Health
Climate, Ecology, and Human Health

... Environmental conditions, interacting with the biology of disease agents, can exert profound effects. Changes in how land is used affect the distribution of disease carriers, such as rodents or insects, while climate influences their range, and affects the timing and intensity of outbreaks. In this ...
Climate Change in Appalachia:
Climate Change in Appalachia:

... imaginative capacity to represent the world in signs and symbols, it turns out, has the corresponding capacity to change that world irrevocably, and perhaps to destroy it. Thus, five weeks into the semester, we in the class have already discussed predictions of large-scale migrations of climate refu ...
Climate change refers to any significant change in measures of
Climate change refers to any significant change in measures of

... levels of green house gases (GHGs) in the atmosphere are contributing to climate change (as theory predicts). In the coming decades, scientists anticipate that as atmospheric concentrations of GHGs continue to rise, average global temperatures and sea levels will continue to rise as a result and pre ...
In the name of God
In the name of God

... Winter –include –mainly –average –region –mild –patters –change – condition Climate is the average of a …….45……’s weather over a period of time. For example ,it is possible that a……46. ……..day in a city could be sunny and ……47……….but the …….48……..weather tells us that its winters will ……..49………….be ...
Clouds Have Made Fools of Climate Modelers
Clouds Have Made Fools of Climate Modelers

... W/m2/C corresponds to no feedback. (This means if the temperature of the atmosphere were uniformly increased by 1 C and nothing else changed, the top of the atmosphere would radiate 3.3 W/m2 more radiation to space.) The feedback is observed to occur on shorter time scales in response to evaporation ...
Presentation - AC Reynolds High
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aerosols - climateknowledge.org
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ch19 climate change ppt
ch19 climate change ppt

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Envir100Lect808
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ch 19 ppt new
ch 19 ppt new

... • Intergovernmental Panel on Climate Change (IPCC), with 2010 updates, cont. • 1906–2005: Ave. temp increased about 0.74˚C • 1970–2009: Annual greenhouse emissions from ...
173736_INTRODUCTION 12-1-11
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... response to the climatic and cultural change-agents—especially courageous decisions and shared sacrifice—and favorable fortune could make for a better fin de siècle world. This chapter explores ways in which the 21st century could prove to be a bridge toward what Mathew Arnold called “civilization m ...
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... insulates the planet  Compare and contrast the different layers of the atmosphere and present information in small groups.  Model the layers of the atmosphere.  Relate how energy provided by the Sun influences global patterns of atmospheric movement and temperature differences between air, water, ...
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CO2 and Temp ppt

... – What is the normal range of CO2 and temperature variability? How is normal defined in this context? – What is the relationship between CO2 and global temperatures? ...
Earth Systems - Assets - Cambridge University Press
Earth Systems - Assets - Cambridge University Press

... town, as if it were about to devour the town. The more recent photographs show the glacier at some distance from the town, quite a distance up the mountains in the background. What accounts for this dramatic retreat in the century after 1855? One hundred and fifty years ago, the global climate was c ...
alexander b. polonsky
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... estimation using the Beaufort scale. It results in artificial positive trends (see for example, [Isemer and Hasse, 1991]). Actually, wind speed data, obtained using the Beaufort scale, underestimate the wind speed. The instrumental measurements began at the end of the 1940's, their fraction in total ...
Assessing and predicting regional climate change
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... be drawn is – if the data collection exercise would be repeated, then we may expect to see again a similar trend. • Example: N European warming trend April – July as part of the seasonal cycle. ...
Climate Change - Caritas Australia
Climate Change - Caritas Australia

... 37 percent. Methane (NH4) has increased by 150 percent and nitrous oxide (N2O) by 18 percent. This rapid increase is more than can be accounted for by natural processes. At the same time that scientists have documented these increases, they have also documented the amounts of greenhouse gases human ...
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... Assumes that the most stable molecular shape has the electron pairs surrounding a central atom as far away from one another as possible ...
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... It should be noted that some definitions of geo-enigineering suggest that only activities that aim to reduce historical emissions should be considered geoengineering whereas those actions that intend to offset present emissions would not be considered as geo-engineering as they don’t result in a net ...
Exploring Climate Change
Exploring Climate Change

... accumulates faster than it melts. The snow changes to ice and slowly moves downhill. Scotland was shaped by glaciers in the last Ice Age, ending about 10,000 years ago. Glaciers cut deep valleys, carved corries and dumped huge amounts of debris when they melted. Both Edinburgh and Glasgow owe much o ...
Hydrologic Effects of Climate Change in the Sierra
Hydrologic Effects of Climate Change in the Sierra

Fact Sheet - Climate Change 2013
Fact Sheet - Climate Change 2013

... The IPCC’s Fifth Assessment Report (AR5) contains contributions from three Working Groups. Working Group I assesses the physical science basis of climate change. Working Group II assesses impacts, adaptation and vulnerability while Working Group III assesses the mitigation of climate change. The Syn ...
wmo support to implementation of the paris agreement
wmo support to implementation of the paris agreement

... Parties should strengthen their cooperation on enhancing action on adaptation, taking into account the Cancun Adaptation Framework, particularly item (c) paragraph 7 of Article 7, “Strengthening scientific knowledge on climate, including research, systematic observation of the climate system and ear ...
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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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