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Arctic approach - ConocoPhillips Norway
Arctic approach - ConocoPhillips Norway

Heat Turn Down the Confronting
Heat Turn Down the Confronting

... will lead to less water resources in summer months and high risks of torrential floods. In the Balkans, a higher risk of drought results in potential declines for crop yields, urban health, and energy generation. In Macedonia, yield losses are projected of up to 50 percent for maize, wheat, vegetabl ...
English
English

Climate Change and Extreme Weather Events
Climate Change and Extreme Weather Events

... emitted by the Earth and keep the planet warmer than it would be otherwise. The mean global temperature, about 15oC, would be far below zero without this natural greenhouse effect. ...
Recent radical shifts of atmospheric circulations and rapid changes
Recent radical shifts of atmospheric circulations and rapid changes

... Arctic storm activity, given the correspondence between the centers of action and the maximum storm activity [e.g., Zhang et al., 2004]. [7] The atmospheric circulation pattern shift is not always in a stable state. The poleward center of action shifted continuously northeastward from 65.0°N, 18.0°W ...
Mapping the return periods of extreme sea levels: Allowing for short
Mapping the return periods of extreme sea levels: Allowing for short

Global Change: Climate Alteration and Global
Global Change: Climate Alteration and Global

Chapter 5 – Sea/Air Interactions
Chapter 5 – Sea/Air Interactions

Gulf Coast Wetland Sustainability in a Changing Climate
Gulf Coast Wetland Sustainability in a Changing Climate

... Mexico (Energy Information Administration, 2007). In 2004, shipping ports in the Gulf states (Texas, Louisiana, Mississippi, Alabama, and Florida) accounted for 49 percent (by tonnage) of all waterborne cargo entering and leaving the United States (U.S. Army Corps of Engineers, 2006). Texas and Lou ...
Role of Ocean in Global Warming - J
Role of Ocean in Global Warming - J

- Arctic Monitoring and Assessment Programme
- Arctic Monitoring and Assessment Programme

... Illustration and Photography Credits ...
Mid ocean ridge worksheet
Mid ocean ridge worksheet

... Mid-Ocean Ridges 1. In what year did scientists discover mid-ocean ridges? 213  ________________________________ 2. Summarize how scientists were able to map out the ocean floor. 213  ________________________________________________________ ________________________________________________________ ...
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Changes in subduction in the South Atlantic Ocean during the

Polar Bears on Ice - Canadian Geographic Education
Polar Bears on Ice - Canadian Geographic Education

Global warming is the increase in the average temperature of Earth`s
Global warming is the increase in the average temperature of Earth`s

Optical Properties of Aerosol Mimics
Optical Properties of Aerosol Mimics

IPCC Asia - Climate Change and Food Security
IPCC Asia - Climate Change and Food Security

Analyzing Vulnerability of the Belize Coastal Tourism Sector
Analyzing Vulnerability of the Belize Coastal Tourism Sector

... of natural hazards) impacts. Secondly, it is a function of sensitivity of the region to them. The sensitivity could be environmental (e.g. land use), human (e.g. social structure), and/or economic (e.g. income per capita). Finally, exposure is correlated with adaptive capacity and adaptation in the ...
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5. Determining vulnerability to climate change

State of the Climate - India Environment Portal | News, reports
State of the Climate - India Environment Portal | News, reports

17 PC Review Exam 2
17 PC Review Exam 2

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Original File - National Snow and Ice Data Center

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Chapter 14--Part 3

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Assessing Public Transportation Vulnerability to Sea Level Rise: A Case Study Application
Assessing Public Transportation Vulnerability to Sea Level Rise: A Case Study Application

melt pond ice foreca..
melt pond ice foreca..

< 1 ... 26 27 28 29 30 31 32 33 34 ... 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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