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New York Times - City Tech OpenLab
New York Times - City Tech OpenLab

02 Antarctica and climate change_Feb14 v3.indd
02 Antarctica and climate change_Feb14 v3.indd

Sea Level Rise and Storm Surge
Sea Level Rise and Storm Surge

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PDF

GLOBAL WARMING AND GLACIERS MELTING AT FJORDS IN
GLOBAL WARMING AND GLACIERS MELTING AT FJORDS IN

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The West Antarctic Ice Sheet in the Fifth Assessment Report of the

... In the recently published AR5, the authors continued to grapple with high uncertainty relating to dynamical changes in the ice sheet. However, they attempted to manage this differently than in AR4 and included a wider breadth of information. Also, there have been strides made in understanding the cl ...
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An Uncertain Introduction

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Prime Meridian

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Global Warming--Gillis et al.

... interview with President Obama in Rolling Stone in which he said that Canada would exploit the oil in its vast tar sands reserves “regardless of what we do.” If Canada proceeds, and we do nothing, it will be game over for the climate. Canada’s tar sands, deposits of sand saturated with bitumen, cont ...
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Presentation

Find some land, build a house?
Find some land, build a house?

... A vast expanse of western Sibera is undergoing an unprecedented thaw that could dramatically increase the rate of global warming, climate scientists warn today. Researchers who have recently returned from the region found that an area of permafrost spanning a million square kilometres - the size of ...
How will this impact people in the USA?
How will this impact people in the USA?

... Fire's potent and pervasive effects on ecosystems and on many Earth processes, including climate change, have been underestimated, according to a new report. "We've estimated that deforestation due to burning by humans is contributing about one-fifth of the human-caused greenhouse effect -- and that ...
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Did scientists predict an impending ice age in the 1970s?

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How are Open-‐Ocean Dynamic Sea Level

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Global Warming-Possible Courses of Action

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Climate Change

... artificially changing natural processes of the Earth.  One idea is to combat warming by blocking some of the sunlight entering the Earth’s atmosphere. ...
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Urban Climate

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nancy-bertler-october-2016 - Goethe Society Wellington

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Notes on Main Ideas and Supporting Evidence

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OTBA material for class VIII - Kendriya Vidyalaya Anantapuram

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Are the oceans Rising NY Times 2010Hazard Variability

... melt. Prevailing winds on the oceans, thermal expansion of warmer waters and melting glaciers also play roles. For that reason, scientists are modeling those different aspects of sea level rise to piece together the entire picture. “The effect of ocean currents and prevailing winds on seal level is ...
The Cocktail to Conversation Guide Global Warming
The Cocktail to Conversation Guide Global Warming

Lecture 36 Anthropogenic Effects on Climate
Lecture 36 Anthropogenic Effects on Climate

... areas, 25% over remote NH oceans from wind transport of aerosols, and imply indirect effect is as big as direct effect. • Overall effect of aerosol is to cancel 20-50% of the radiative impact of greenhouse gas. Large uncertainty about aerosol absorption, indirect effect. • If man stopped producing a ...
Weather EXTREMES - Department of Meteorology and Climate
Weather EXTREMES - Department of Meteorology and Climate

... 20-Year Trends in Arctic Sea Ice Coverage Yearly and Seasonal Ice Coverage Trends ...
Climate change - is it really happening
Climate change - is it really happening

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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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