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Climate Reconstruction from Subsurface Temperatures
Climate Reconstruction from Subsurface Temperatures

... indicators from the continents and some oceanic islands. There are, of course, important meteorologic observations over longer time periods in a few selected areas, but it was not until the latter decades of the nineteenth century that geographic coverage was widespread in both the northern and sout ...
Folie 1 - hvonstorch.de
Folie 1 - hvonstorch.de

... After World War II it was speculated whether a cooling was the first indication of a new Ice Age, possibly brought on by human pollution. Schneider (1971) speculated that human pollution would increase by a factor of up to 8 which could increase the opacity of the atmosphere within hundred years by ...
Bell Ringer
Bell Ringer

... define changing trends in the Earth’s climate.  Scientists used to refer to the trend in increasing thermal energy as global warming. However, this is not an accurate picture of all of the effects of this phenomenon.  We now define this trend as climate change, since there are effects well beyond ...
Diurnal temperature range as an index of global
Diurnal temperature range as an index of global

... data since 1901. The effect of missing data within any individual year for individual grid boxes had very little impact on the annual mean. We used a fixed data mask rather than a temporally-varying mask as changes in globalmean DTR were found to be relatively insensitive to time variations in the d ...
EVSC 305: Climate Change – the Science and
EVSC 305: Climate Change – the Science and

... ◦ Will climate change dissipate clouds, which would effectively speed up the process of climate change, or increase cloud cover, which would slow it down? ◦ One study (July 2009, Science) level clouds tend to dissipate as the ocean warms — which means a warmer world could well have less cloud cover. ...
The Impact of Climate Change on Insurance against Catastrophes
The Impact of Climate Change on Insurance against Catastrophes

... There are opportunities for new business strategies, which create value, encourage sustainable behaviour in society and mitigate against further climate change. There is also scope for research into adaptation strategies whereby vulnerability to more frequent or more intense events could be minimise ...
BURMA - Climatelinks
BURMA - Climatelinks

... Burma, also called Myanmar, is a mountainous country in Southeast Asia with an extensive coastline and an estimated population of 51.4 million people. The country is inherently prone to extreme weather events, including floods, cyclones, tsunamis, heavy monsoon rains, floods, storm surges and drough ...
Global Warming - Department of Geology UPRM
Global Warming - Department of Geology UPRM

... Greenhouse effectThe "greenhouse effect" is the warming that happens when certain gases in Earth's atmosphere trap heat. These gases let in light but keep heat from escaping, like the glass walls of a greenhouse.First, sunlight shines onto the Earth's surface, where it is absorbed and then radiates ...
Neymar, Serena Williams and Kolo Touré join
Neymar, Serena Williams and Kolo Touré join

Effect of outdoor temperature, heat primes and anchoring on belief
Effect of outdoor temperature, heat primes and anchoring on belief

... time understanding the risks of global warming conveyed in scientific publications such as those prepared by the Intergovernmental Panel on Climate Change (Budescu, Broomell, & Por, 2009). Given the latter, Budescu and colleagues have argued that “.social scientists specializing in risk assessment an ...
Climate and greenhouse gases
Climate and greenhouse gases

... As shown in Figure 2.3, feedback processes connect the atmospheric levels of GHGs (CO2, methane, and others), water vapour, cloudiness, the extent of polar ice caps, and global temperature. The global average concentration of water vapour quickly increases in response to an increase in global temper ...
Vol.5, No.2, 2005
Vol.5, No.2, 2005

... ainfall over the Indonesian region has a pronounced diurnal signature. One test of how well moist convection is represented in models is how well the diurnal rainfall cycle is simulated in this region. In typical atmospheric circulation models, the rainfall over the Maritime Continent peaks too earl ...
a system with dangerous thresholds?
a system with dangerous thresholds?

... periments, including the causes for differences or apparent contradictions between models. Many early model studies were performed with ocean-only models with nearly fixed sea surface temperature (SST), neglecting the feedback of the ocean circulation on SST. This distorts the parabola in Figure 2 i ...
- OceanObs`09
- OceanObs`09

... computing facilities that will enable the revolution in climate prediction by supporting the model resolution and complexity required for the most advanced and reliable representations of the climate system that technology and our scientific understanding of the problem can deliver. This computing c ...
Climate Change
Climate Change

... Polar Science Center researchers observe and model the physical processes that control the nature and distribution of sea ice and polar ice sheets, the structure and movement of high-latitude oceans, and the interactions between air, sea, ice and biota. The Center has made major contributions to the ...
1 CATASTROPHE TRENDS Lloyd’s
1 CATASTROPHE TRENDS Lloyd’s

Environmental Change of Trans International Boundary Indo
Environmental Change of Trans International Boundary Indo

... Fig.5. Top Albedo Maps The albedo at the top of the atmosphere ( computed as follows: ...
Air Pollution, Climate Change, and Ozone Depletion
Air Pollution, Climate Change, and Ozone Depletion

... Nitrous Oxide (N2O) ...
Paleoclimate Implications for Human-Made Climate Change
Paleoclimate Implications for Human-Made Climate Change

... The Cenozoic era illustrates the huge magnitude of natural climate change. Earth was so warm in the early Cenozoic that polar regions had tropical-like conditions – indeed, there were alligators in Alaska (Markwick, 1998). There were no large ice sheets on the planet, so sea level was about 75 meter ...
The ocean`s role in polar climate change: asymmetric Arctic and
The ocean`s role in polar climate change: asymmetric Arctic and

... phenomenon known as Arctic amplification). Since 1979, the beginning of the reliable satellite record, Arctic summer sea-ice extent has decreased by order 12% per decade, with smaller reductions in winter. Coupled models suggest that under greenhouse gas (GHG)-induced warming, the Arctic will warm t ...
Climate Change and Politics
Climate Change and Politics

... Change As the world’s population continues to grow (an increase of over a billion people in just the past 12 years), migratory pressures become a major concern and a reality Libya is cooperating with the EU in a multi billion project to prevent the further migration of unwanted refugees to Europe Wh ...
"The Response of Dissolved Oxygen to Climate and Other Anthropogenic Change"
"The Response of Dissolved Oxygen to Climate and Other Anthropogenic Change"

the PDF - Sustainablecorn.org
the PDF - Sustainablecorn.org

... Corn is currently grown on more than 20 percent of total U.S. cropland and is the dominant crop in the Midwest region, most often in rotation with soybean. The highly versatile crop is an economic powerhouse, employing millions and producing food, feed and fuel for use by every citizen. With demand ...
PowerPoint Lecture - UCSD Department of Physics
PowerPoint Lecture - UCSD Department of Physics

... • Adding CO2 to the atmosphere changes the radiative balance on earth – CO2 absorbs infrared light, so more of the thermal emission trying to escape from earth is absorbed in the atmosphere, causing earth to warm – it’s like the glass sheet over the solar hot water collector: like a greenhouse – eve ...
SorceMeetingNotes
SorceMeetingNotes

... Raschke showed discrepancies in GCM’s downward solar flux – embarrassing (Global Climate Modelers – we have only one Sun) Clouds, Radiation, and Climate – largest uncertainty in global climate sensitivity over the next century is CLOUD FEEDBACK – can amplify or dampen global warming Cloud feedback s ...
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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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