• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
The pros and cons of Cardiff Bay
The pros and cons of Cardiff Bay

Muller2012-TheConversionofaClimate-ChangeSkeptic-+
Muller2012-TheConversionofaClimate-ChangeSkeptic-+

Tuvalu: first casualty of climate change
Tuvalu: first casualty of climate change

Do now! - MrSimonPorter
Do now! - MrSimonPorter

... ages. They imply that the threat of a new ice age must now stand alongside nuclear war as a likely source of wholesale death and misery for mankind. (Nigel Calder, former editor of New Scientist, in International Wildlife, July 1975) The cooling has already killed thousands of people in poor nations ...
New Zealand Climate Change Research Institute
New Zealand Climate Change Research Institute

... of extreme events At a meeting of climate scientists covering extreme events in August 2010, Kevin Trenberth gave a detailed explanation of potential connections between:  Arctic ice sheet loss,  warming of the Indian Ocean,  blocking of weather patterns over much of Asia,  record droughts in Ru ...
Slide 1
Slide 1

... Thickness of atmospheric layers exaggerated for clarity. ...
PHILIP ALLAN UPDATES - SLC Geog A Level Blog
PHILIP ALLAN UPDATES - SLC Geog A Level Blog

... plonked a flag on the seabed under the North Pole, and lodged a claim of sovereignty with the United Nations. Protestations apart, Canada has hardly been idle itself in the Arctic. In its own show of strength, in July it announced it would spend a hefty US$7 billion patrolling the Arctic Circle with ...
Theme 2 – Climate Change
Theme 2 – Climate Change

ppt converted from keynote - Hans
ppt converted from keynote - Hans

Prehistoric Era Overview
Prehistoric Era Overview

Impacts of warming
Impacts of warming

... Land ecosystems and agriculture: A warming world combined with changes in the amount of carbon dioxide in the atmosphere (with increases potentially enabling faster growth of vegetation) presents a more complex picture for future impacts on crop yields and ecosystems such as forests, as well as the ...
1. Which of the following are greenhouse gases?
1. Which of the following are greenhouse gases?

iced - clivar
iced - clivar

... The marine cryosphere and its interactions with high latitude oceans and atmosphere What will be the nature of changes in sea-ice distribution and mass balance in both polar regions in response to climate change and variability? ...
Earth`s Climate System Today
Earth`s Climate System Today

... Variations of Earth’s surface temperature for the past 1000 years ...
Global Warming: The Scientific Basis for Anthropogenic Climate
Global Warming: The Scientific Basis for Anthropogenic Climate

... 18 to 59cm by 2100. A further 10 to 20cm may occur due to melting of ice sheets. • However further ice sheet contributions cannot be discounted or at present quantified. • 20,000 yrs BP when temperatures were 4 to 7°C less than present sea level was 120m below present. • In the Pliocene 3 million ye ...
co2_impact_on_climate - Colorado Professional Learning
co2_impact_on_climate - Colorado Professional Learning

Climate Change - Cloudfront.net
Climate Change - Cloudfront.net

Notable scientific and societal landmarks: 1985
Notable scientific and societal landmarks: 1985

unit_6_climate_change
unit_6_climate_change

... Zooplankton in parts of California Current have decreased by 80% since 1951 ...
Tues Jan 6 - UW Atmospheric Sciences
Tues Jan 6 - UW Atmospheric Sciences

available for here - Office of the Prime Minister`s Chief
available for here - Office of the Prime Minister`s Chief

Higher Geography
Higher Geography

Key drivers of climate change can be global and local
Key drivers of climate change can be global and local

Global Climate Change Fact Sheet - Minnesota Pollution Control
Global Climate Change Fact Sheet - Minnesota Pollution Control

Biota in Danger
Biota in Danger

... * Humans are responsible for fastest rate of extinction since dinosaurs * Human beings continue to dominate "Survivor: Earth," voting other species off the island at a blistering pace. "In effect, we are currently responsible for the sixth major extinction event in the history of earth, and the grea ...
< 1 ... 85 86 87 88 89 90 91 92 93 ... 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.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report