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Presentation Part 2
Presentation Part 2

... • Recognizing the vulnerability to the impacts of climate change and climate variability on the economic development and social needs of the region: – The Heads of Governments of CARICOM member states in July 2002, endorsed the creation of a permanent capacity in the region to address climate change ...
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What we do not know in terms of adaptation

... A recent paper by Oreskes et al. in the journal Philosophy of Science asserts that “there is a gap between the scale on which models produce consistent information and the scale on which humans act”. While the large scales, such as the global mean, provide the best indicators of the state of earth’s ...
Global Warming - Year 10 Life Science
Global Warming - Year 10 Life Science

... 1993 to 2012. Rates of sea level rise are not uniform around the globe and vary from year to year. Since 1993, the rates of sea level rise to Australia’s north and northwest have been 7 to 11 millimetres per year, with rates of sea level rise on the central east and southern coasts between 2 to 5 mi ...
Extreme weather events and climate change
Extreme weather events and climate change

... This year the World Metrological Organisation published a report called ‘The Global Climate 20012010: a decade of climate extremes’1. In it they pointed to a twenty per cent increase in lives lost in extreme weather events compared to a decade earlier. Over 350,000 lives were lost globally due to ex ...
Costs and Benefits of Reducing Greenhouse Gas Emissions
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... The Economics of Climate Change: Costs and Benefits of Reducing GHG Emissions Maureen Cropper University of Maryland and Resources for the Future August 26th 2010 ...
Climate Change - Western Kentucky University
Climate Change - Western Kentucky University

... Islands damage in 2004 possible harbinger of future INNOVATIVE ADAPTION NEEDED ...
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Spring 2005

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... In May 1996, two leading IPCC scientists – Dr. Benjamin Santer and Dr. Tom M. L. Wigley – explained the pivotal findings of a new IPCC report to a packed Congressional office in Washington, DC. These results, published one month later in Nature22, were described by the journal as “the clearest evide ...
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... ensembles of intermediate-complexity models1,2 and estimates of the strength of carbon-cycle feedbacks13 . From this evidence it is clear that the CMIP-3 ensemble, which represents a valuable expression of plausible responses consistent with our limited ability to explore model structural uncertaint ...
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... being studied. In this activity, the continuous average of a cluster of data (a 10-year span of temperature records) yields more meaningful information about temperature trends than a single data set (a one-year span of monthly temperature records) provides. A single data set is more likely to conta ...
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... has added a huge amount of fresh water already. Meanwhile, rivers are pouring up to 10 per cent more water into the ocean than they did half a century ago. This is partly the result of rising precipitation as the air warms - warmer air can hold more moisture - and partly the result of melting permaf ...
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Climate Change and Human Health

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... direct causal link to global warming has been established for some observed changes, such as sea-level rise and worldwide glacial retreat, such a link is difficult to definitively establish for other changes, such as the increased incidence of droughts or the migration of a particular species. Howev ...
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... Governor Schwarzenegger in 2005,[4] set a much more ambitious ultimate goal as well: an 80% reduction from 1990 levels, to be achieved by 2050. The 2050 target remains the policy of the state but has not been codified to date. With the 2020 standard in sight as well as in reach, the 2050 standard ha ...
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... temperature, the earth has to return the energy it receives back to space, primarily as heat. Clouds alter the energy flow in both directions. On balance, in today’s climate, clouds cool the earth. Dense, low-lying clouds are responsible for most of that effect, because they reflect considerable sun ...
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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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