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... But it has also been subject to criticism as it is much more political. In principle, this process is designed to provide a report in which the content is determined by the science while how it is stated is determined jointly with the governments. Hence it aids communication between scientists and p ...
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 ...
Frequently Asked Questions about Global Warming
Frequently Asked Questions about Global Warming

Paleooceanography and Sea
Paleooceanography and Sea

... • The other features that are prominent in this photograph are the dark circular patches. • These represent the surface expression of salt domes that have risen diapirically from the Cambrian Hormuz salt horizon through the younger sediments to reach the surface. – Only in a hot arid environment su ...
Wake HM 1AR v MSU HR Ky semis
Wake HM 1AR v MSU HR Ky semis

... Continuing a decade-long trend of declining global temperatures, the year 2008 was significantly colder than 2007, and global temperatures for the year were below the average over the past 30 years. The global temperature data, reported by NASA satellite-based temperature measurements, refuted predi ...
Melting Away - Global Warming
Melting Away - Global Warming

Earthday_flyer
Earthday_flyer

... Dr. Axel Timmerman, Professor in Physical Oceanography at the University of Hawai’i, is well known for his scientific studies on past and future climate change. He has published more than 100 papers on a wide range of topics, including the El-Niño Southern Oscillation, Ice Ages, and abrupt Climate C ...
Towards advanced understanding and
Towards advanced understanding and

... the Total Heat Flux across Chukchi Shelf Line ...
Changes in the Global Water Cycle Linked to Global Warming
Changes in the Global Water Cycle Linked to Global Warming

Climate Change, Tipping Points, and the Media
Climate Change, Tipping Points, and the Media

- Sustainable Loudoun
- Sustainable Loudoun

the full interview as a Word file.
the full interview as a Word file.

Calculation of Greenland and Antarctica Glaciers` Weights Causing
Calculation of Greenland and Antarctica Glaciers` Weights Causing

Chapter 3 Powerpoint
Chapter 3 Powerpoint

... Mauna Loa observations, the concentration of carbon dioxide appears to be increasing over time. ...
chapter 19 powerpoint1
chapter 19 powerpoint1

... Alley (2000) from GISP2 ice core data. The lower panel shows the past atmospheric CO2 content, as found from the EPICA Dome C Ice Core in the Antarctic (Monnin et al. 2004). The Dome C atmospheric CO2 record ends in the year 1777. www.climate4you.com ...
Medieval Warm Period - Natural Climate Change
Medieval Warm Period - Natural Climate Change

... prior to the instrumental record were not that well known or understood. Fifteen years later, understanding is much improved, more quantitative and better integrated with respect to observations and modeling”. ...
Document
Document

Global Warming and Human Health
Global Warming and Human Health

Chapter 21 Outline Ozone
Chapter 21 Outline Ozone

... troposphere, or a cooling effect by reflecting more sunlight back into space. 2. Several factors will affect the net result of more cloud cover such as the amount of water vapor in the troposphere, whether clouds are thin or thick, coverage, altitude of the cloud, size and number of water droplets, ...
Future prospective of Global warming on Invertebrates and
Future prospective of Global warming on Invertebrates and

nsu-2005-11-17
nsu-2005-11-17

... theory is correct then instruments should have recorded a bigger temperature rise for calm nights than for windy ones, because wind blows excess heat away from cities and away from the measuring instruments. There was no difference between the calm and windy nights, and the author says: we show that ...
FINAL EXAM: MONDAY MARCH 17 3-6PM
FINAL EXAM: MONDAY MARCH 17 3-6PM

... Weather: Atmospheric state at a particular time Climate: Weather averaged over many times (30 or more) ...
01_02 Chavez
01_02 Chavez

NORCLIM (IPY 120): Northern High Latitude Climate variability
NORCLIM (IPY 120): Northern High Latitude Climate variability

Global Warming and Human Health
Global Warming and Human Health

... animals who inhabit the same areas as these polar ice caps to loose part of their habitats Weather patterns- Weather patterns will greatly be affected by global warming as the weather must take into account a warmer climate Wetlands- As sea levels rise due to global warming the number of wetlands di ...
< 1 ... 74 75 76 77 78 79 80 81 82 ... 105 >

Future sea level



The rate of global mean sea-level rise (~3 mm/yr; SLR) has accelerated compared to the mean of the 20th century (~2 mm/yr), but the rate of rise is locally variable. Factors contributing to SLR include decreased global ice volume and warming of the ocean. On Greenland, the deficiency between annual ice gained and lost tripled between 1996 and 2007. On Antarctica the deficiency increased by 75%. Mountain glaciers are retreating and the cumulative mean thickness change has accelerated from about −1.8 to −4 m in 1965 to 1970 to about −12 to −14 m in the first decade of the 21st century. From 1961 to 2003, ocean temperatures to a depth of 700 m increased and portions of the deeper ocean are warming.The Intergovernmental Panel on Climate Change (2007) projected sea level would reach 0.18 to 0.59 m above present by the end of the 21st century but lacked an estimate of ice flow dynamics calving. Calving was added by Pfeffer et al. (2008) indicating 0.8 to 2 m of SLR by 2100 (favouring the low end of this range). Rahmstorf (2007) estimated SLR will reach 0.5 to 1.4 m by the end of the century. Pielke (2008) points out that observed SLR has exceeded the best case projections thus far. These approximations and others indicate that global mean SLR may reach 1 m by the end of this century. However, sea level is highly variable and planners considering local impacts must take this variability into account.
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