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Powerpoint file for Chapter 1 (Introduction)
Powerpoint file for Chapter 1 (Introduction)

... broad agreement in indicating that the climate sensitivity is highly likely (say, 90% probability) to lie between 1.5ºC and 4.5ºC. That is, we expect each CO2 doubling (or its radiative equivalent) to eventually warm the climate by 1.5-4.5 C in the global mean. ...
Abstracts of Global Warming and Climate Change
Abstracts of Global Warming and Climate Change

... The world’s climate scients have reported that the earth’s climate system is increasingly heating up and it likely has not been this warm for at least 13000 years. Heating effects are strong in melting of snow and ice, rising global mean sea level, widespread changes in precipitation amounts, ocean ...
Recent climate change in the Baltic Sea region
Recent climate change in the Baltic Sea region

Word format
Word format

... There are many factors of natural variability including geological processes. Atmospheric chemistry changes are secondary to these drivers of climate change. The effects on sea level rise of the West Antarctic Ice Sheet collapse are significant and also drives changes in ocean currents and conseque ...
Maximum CO2 Will Warm Earth for 20
Maximum CO2 Will Warm Earth for 20

Climate Control and Ozone Depletion
Climate Control and Ozone Depletion

... • Tipping point – the irreversible estimated threshold for large scale climate changes – CO2 levels exceeding 450 ppm – In 2007 CO2 levels were 384 ppm ...
Cecilie Mauritzen, CICERO Large Developing Economies: 2010-2013
Cecilie Mauritzen, CICERO Large Developing Economies: 2010-2013

Ch. 20
Ch. 20

... troposphere can decrease the ability of the ocean to remove and store CO2 by decreasing the nutrient supply for phytoplankton and increasing the acidity of ocean water.  Global warming will lead to prolonged heat waves and droughts in some areas and prolonged heavy rains and increased flooding in o ...
Export - NCEAS Computing Services Knowledge Base
Export - NCEAS Computing Services Knowledge Base

... This will be important to bear in mind as we work through the kinds of questions we need to answer, as well as what sampling methods and designs will work into the future. Below are some highlights of the recent lit review I did as part of a Draft Environmental Impact Statement for Western Oregon. M ...
Global warming: At what point does atmospheric greenhouse gas
Global warming: At what point does atmospheric greenhouse gas

... way of life but ultimate future existence on this planet. Global warming is defined as the steady mean increase in atmospheric temperature, the primary asserted cause thereof being increased emissions and inherent atmospheric concentrations of “greenhouse gases” – carbon dioxide in particular. These ...
Analysis of winter and summer warming rates in
Analysis of winter and summer warming rates in

... Hemisphere, winters are warming much more quickly than summers over the continental surfaces according to the IPCC database. The results using the 100 yr temperature record are similar to those using the 50 yr record, even though only 546 grid cells contain at least 90% available data for the period ...
Wage   et to fall unle     warming i   tackled
Wage et to fall unle warming i tackled

General Overview of Climate Change Science
General Overview of Climate Change Science

climate change ppt
climate change ppt

... Age included severe storms, wet periods, dry periods, extreme hot and cold conditions - Viking settlements abandoned in Greenland Little Ice Age in Spain  ...
lesson 5 materials
lesson 5 materials

... Big Ideas of Lesson 5 Unit 5 • Using fossil fuels to create energy results in the emission of greenhouse gases which contribute to global warming. • Global warming has resulted in climate change. • Continued global warming can have many negative effects on the environment including rising ocean leve ...
Chapter 20 Power Point
Chapter 20 Power Point

... warmer troposphere can decrease the ability of the ocean to remove and store CO2 by decreasing the nutrient supply for phytoplankton and increasing the acidity of ocean water.  Global warming will lead to prolonged heat waves and droughts in some areas and prolonged heavy rains and increased floodi ...
MSWord
MSWord

... The changes are more rapid than could be explained by long-term natural variability, and yet more sustained than could be caused by short-term natural events; The changes occur on a global scale, unlike some previous patterns that occurred only regionally. ...
Slide 1
Slide 1

... Conference on Reduction of vulnerability of West Africa to climate change Ouagadougou, January 24-27 2007 ...
What will climate change look like?
What will climate change look like?

... There will also be more extreme weather events. But it doesn’t feel warmer! It is often difficult to reconcile the recent cold, wet summers with the fact that the ten warmest years on record have all occurred since 1994. However, what sticks in our minds is short term weather rather than long term t ...
UN & GLOBAL WARMING
UN & GLOBAL WARMING

... growing conciousness and willingness on the part of the public to accept and encourage environmental policy and legislation.  The 'E.U Sustainable Development Strategy (SDS)' was established to answer exactly that question  So the E.U - acknowledging its role within the world's sphere champions th ...
Higher Geography - Atmosphere
Higher Geography - Atmosphere

presentation - Globelics Academy
presentation - Globelics Academy

... The Science of Climate Change GHGs and global warming (the greenhouse effect)  Initial doubts about the validity of the theory largely gone, but still some critics exist  Global consensus among climate scientists  How does the scientific enterprise work? ...
When researching back and looking at some of the things we need
When researching back and looking at some of the things we need

... world. By reflecting sunlight back into space, Arctic ice prevents the heating of the Earth’s surface. However, when ice melts (due to global warming), it leaves behind bare soil or open waters, both of which absorb more solar energy than ice. This extra heat melts even more ice. Less ice means less ...
There were times in the past when little permanent ice existed on
There were times in the past when little permanent ice existed on

... attribution of the term at regional scales is complicated by significant regional variations in temperature changes due to the influence of modes of climate variability such as the North Atlantic Oscillation and the El Nino/Southern Oscillation. Indeed, the utility of the term in describing past cli ...
The global warming hiatus: Slowdown or redistribution?
The global warming hiatus: Slowdown or redistribution?

... original work is properly cited, the use is non-commercial and no modifications or adaptations are made. ...
< 1 ... 362 363 364 365 366 367 368 369 370 ... 438 >

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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