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Safe Climate Policy - Public Health Association of Australia Inc
Safe Climate Policy - Public Health Association of Australia Inc

... 10. A carbon budget gives a method for understanding the effects of atmospheric greenhouse gas (GHG) levels on global warming and climate since it is the cumulative stock of GHGs in the atmosphere that forces total warming. Models estimate that to have a 50 per cent probability of not exceeding 2 de ...
CRITICAL THINKING, THE COMMON GOOD, AND THE NEW
CRITICAL THINKING, THE COMMON GOOD, AND THE NEW

...  Inaction does not serve the common good.  Inaction means natural laws will reduce the human population to or below Earth’s carrying capacity.  Climate change and exponential human population growth are interactive ...
Environmental Questions. Affordable Answers?
Environmental Questions. Affordable Answers?

... electric generating plants. We support a full discussion of all the issues, and we particularly oppose enacting regulations that prevent new coal-fired plants (with modern technology) from being built. Coal is still—by far—our most plentiful and economical source of energy. More research about the e ...
climate change as a major geological event
climate change as a major geological event

PDF file: Impacts of climate change on arable crops – adaptation
PDF file: Impacts of climate change on arable crops – adaptation

Slide 1
Slide 1

... 1. Chief instigator of climate change was earth orbital change, a very weak forcing. 2. Chief mechanisms of Pleistocene climate change are GHGs & ice sheet area, as feedbacks. 3. Climate on long time scales is very sensitive to even small forcings. 4. Human-made forcings dwarf natural forcings that ...
Impact of the global warming hiatus on Andean temperature
Impact of the global warming hiatus on Andean temperature

Regional_Economic_Gr.. - Erasmus Mundus Students and Alumni
Regional_Economic_Gr.. - Erasmus Mundus Students and Alumni

... While we may have scientific and rhetorical consensus today, real costs have not yet been taken on. - what is the resilience of CC mitigation strategies / institutions in the medium term? We may have occasional visionary leaders, but they don't stick around forever - we need incentives to maintain p ...
3.2 St Pauls Climate Change assessment File
3.2 St Pauls Climate Change assessment File

Met 10
Met 10

...  IPCC-Intergovernmental Panel on Climate Change – Greenhouse gas concentrations continue to rise (warming). – Anthropogenic aerosols tend to produce negative radiative forcing (cooling) “The balance of evidence suggests a discernible human influence on global climate” (IPCC) 1997 "There is new and ...
Climate change: The Need to Consider  g Human Forcings in Addition to  h
Climate change: The Need to Consider  g Human Forcings in Addition to  h

Multidecadal Meridional Overturning Circulation Variability and
Multidecadal Meridional Overturning Circulation Variability and

... MOC may respond to the multidecadal changes ...
Amy Clement - University Corporation for Atmospheric Research
Amy Clement - University Corporation for Atmospheric Research

... School of Marine and Atmospheric Science at the University of Miami. She is the 2007 recipient of the James B. Macelwane Medal of the American Geophysical Union, awarded for “significant contributions to the geophysical sciences by a young scientist of outstanding ability.” In her research, Dr. Clem ...
Document
Document

... hence are not impelled to act. In addition trust in these institutional actors is low – In turn politicians want people to act, while at the same time see the electoral cycle as a reason to not impose what they see as unpopular environmental measures – Resolving the perceptions on both side of this ...
Questions for Illustrated Text Video 1) How does the video introduce
Questions for Illustrated Text Video 1) How does the video introduce

... 22) Do nitrogen and oxygen gas add to the greenhouse effect? Explain. 23) What are the four main greenhouse gases? 24) Which is by far the most important greenhouse gas? Why? Part III. Carbon Dioxide (5:20) 25) Where did CO2 come from in the early Earth, half billion years ago? 26) How was CO2 from ...
Annex N Sunflowers and Climate Change
Annex N Sunflowers and Climate Change

... fourth assessment (4AR) of the International Panel on Climate Change (IPCC) ‘warming of the climate system is unequivocal, as in now evident from observations in global average air and ocean temperatures, widespread melting of snow and ice, and rising global temperatures’ (IPCC, 2007, 1). The global ...
Media Release
Media Release

... “The next step is to correlate past, present and likely future influences on the marine ecosystem and extend our studies into risk and mitigation options, particularly where there are social, economic and environmental interests at the coasts and in our iconic marine parks,” Dr Lenton said. The thre ...
National Geographic - u.arizona.edu
National Geographic - u.arizona.edu

... Rising sea level is not the only change Earth's oceans are undergoing. The ten-year-long World Ocean Circulation Experiment, launched in 1990, has helped researchers to better understand what is now called the ocean conveyor belt (see page 66). Oceans, in effect, mimic some functions of the human ci ...
Global Warming: A White Paper on the Science, Policies
Global Warming: A White Paper on the Science, Policies

... this paper is to present a current snapshot of the global warming issue, particularly with respect to the U.S. semiconductor industry. There is a natural greenhouse effect known to keep the mean temperature of the Earth’s atmosphere at about 15°C (60°F). The primary gases responsible for this are wa ...
Elements of climate science- policy interaction in Germany
Elements of climate science- policy interaction in Germany

... interaction in particular regions and on the national/European level ...
Vanishing and Emerging Ecosystems of Coastal Virginia: Climate
Vanishing and Emerging Ecosystems of Coastal Virginia: Climate

... On a global scale, a principal cause of the habitat alteration producing novel ecosystems is climate change,3 which is expected to continue under all realistic scenarios of future population trends and economic activity. For example, in the Chesapeake Bay region, annual average temperatures of surfa ...
Note Making: Reference Sources
Note Making: Reference Sources

... Appears at the end of the work Contains only work cited in text Begins on a new page Continue to number pages even of Works Cited Page number should be in the upper right hand corner/flush with the right margin (1/2 inch from the top) Centre the title Works Cited (one inch from the top) Double space ...
Results from a survey examining college student & adult public
Results from a survey examining college student & adult public

... Quotes from 2012 US Presidential Campaign “More droughts and floods and wildfires are not a joke. My plan will continue to reduce the carbon pollution that is heating our planet because climate change is not a hoax.” ...
Climate Change and Coastal Ecosystems
Climate Change and Coastal Ecosystems

... On a global scale, a principal cause of the habitat alteration producing novel ecosystems is climate change,3 which is expected to continue under all realistic scenarios of future population trends and economic activity. For example, in the Chesapeake Bay region, annual average temperatures of surfa ...
CO2, the greenhouse effect and global warming: from the
CO2, the greenhouse effect and global warming: from the

... Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (Cambridge: Cambridge University Press, 2013). Warming is specified relative to the reference period, 1986–2005, and the figures represent ensemble-mean results of the ESMs. ...
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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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