What if greenland melted




















A memory. Reclaimed by the Adriatic Sea. Thousands of years from now, in this catastrophic scenario, the Netherlands will have long since surrendered to the sea, and most of Denmark will be gone too. Meanwhile, the Mediterranean's expanding waters will also have swelled the Black and Caspian Seas.

Land now inhabited by million Chinese would flood, as would all of Bangladesh, population million, and much of coastal India. Predominantly desert, the continent would gain a new inland sea—but it would lose much of the narrow coastal strip where four out of five Australians now live. East Antarctica: The East Antarctica ice sheet is so large—it contains four-fifths of all the ice on Earth—that it might seem unmeltable.

It survived earlier warm periods intact. Lately it seems to be thickening slightly—because of global warming. The warmer atmosphere holds more water vapor, which falls as snow on East Antarctica. But even this behemoth is unlikely to survive a return to an Eocene Climate. West Antarctica: Like the Greenland ice sheet, the West Antarctic one was apparently much smaller during earlier warm periods. It's vulnerable because most of it sits on bedrock that's below sea level. The warming ocean is melting the floating ice sheet itself from below, causing it to collapse.

Since it has averaged a net loss of 65 million metric tons of ice a year. All rights reserved. This story appears in the September issue of National Geographic magazine. Share Tweet Email. Read This Next Wild parakeets have taken a liking to London. Technical Announcements. Employees in the News. Emergency Management. Survey Manual. There is still some uncertainty about the full volume of glaciers and ice caps on Earth, but if all of them were to melt, global sea level would rise approximately 70 meters approximately feet , flooding every coastal city on the planet.

Currently, the volume of land ice on Earth is decreasing, driving consequential changes to global sea level and local stream habitat. The U. Geological Survey Benchmark Glacier Project conducts glaciological research and collects field Executive SummaryThe U. The southern Chesapeake Bay region is experiencing land subsidence and rising water levels due to global sea-level rise; land subsidence and rising water levels combine to cause relative sea-level rise.

Land subsidence has been observed since the s in the southern Chesapeake Bay region at rates of 1. Coastal areas are essential to the economic, cultural, and environmental health of the Nation, yet by nature coastal areas are constantly changing due to a variety of events and processes. Extreme storms can cause dramatic changes to our shorelines in a matter of hours, while sea-level rise can profoundly alter coastal environments over decades In the other 10 chapters, each of which concerns a specific glacierized region of Earth, the authors used remotely The Alaskan landscape is changing, both in terms of effects of human activities as a consequence of increased population, social and economic development and their effects on the local and broad landscape; and those effects that accompany naturally occurring hazards such as volcanic eruptions, earthquakes, and tsunamis.

Some of the most prevalent The coastline of the United States features some of the most popular tourist and recreational destinations in the world and is the site of intense residential, commercial, and industrial development. The coastal zone also has extensive and pristine natural areas, with diverse ecosystems providing essential habitat and resources that support Geological Survey, in cooperation with the South Carolina Sea Grant Consortium, conducted a 7-year, multidisciplinary study of coastal erosion in northeastern South Carolina.

Shoreline behavior along the coast of Long Bay is dictated by waves, tidal currents, and sediment supply that act within the overall constraints of the regional Fifty years of U. Geological Survey USGS research on glacier change shows recent dramatic shrinkage of glaciers in three climatic regions of the United States.

These long periods of record provide clues to the climate shifts that may be driving glacier change. Glaciers are important features in the hydrologic cycle and affect the volume, variability, and water quality of runoff. Assessing and predicting the effect of glaciers on water resources require a monitoring program to provide basic data for this understanding.

The monitoring program of the U. Geological Survey employs a nested approach whereby Rising sea level is potentially one of the most serious impacts of climatic change.

Even a small sea level rise would have serious economic consequences because it would cause extensive damage to the world's coastal regions. Sea level can rise in the future because the ocean surface can expand due to warming and because polar ice sheets and Most Americans have never seen a glacier, and most would say that glaciers are rare features found only in inaccessible, isolated wilderness mountains.

Are they really so rare? Or are they really potentially important sources of water supply? New U. Geological Survey-led coastal modeling research presents state, federal, and commercial entities with varying storm and sea level-rise scenarios to assist with planning for future infrastructure and mitigation needs along the California coast.

The warming climate has dramatically reduced the size of 39 glaciers in Montana since , some by as much as 85 percent, according to data released by the U.

Geological Survey and Portland State University. As coastal development along the Gulf Coast continues to expand, tidal saline wetlands could have difficulty adjusting to rising sea levels. Islands used by tropical seabirds are highly vulnerable to sea level rise according to a new study released today.

Geological Survey and Oregon State University released a report this week examining Pacific Northwest tidal wetland vulnerability to sea level rise. Scientists found that, while vulnerability varies from marsh to marsh, most wetlands would likely be resilient to rising sea levels over the next years. Frozen bodies of ice cover nearly 10 percent of the state of Alaska, but the influence of glaciers on the environment, tourism, fisheries, hydropower, and other important Alaska resources is rarely discussed.

Communities and coastal habitats in the southern Chesapeake Bay region face increased flooding because, as seawater levels are rising in the bay, the land surface is also sinking. Rates of sea level rise are increasing three-to-four times faster along portions of the U. Atlantic Coast than globally, according to a new U.

Geological Survey report published in Nature Climate Change. The Earth is a watery place. But just how much water exists on, in, and above our planet? About 71 percent of the Earth's surface is water-covered, and the oceans hold about The simulation below reflects the predicted exponential rise in atmospheric CO2 concentrations, a 2xCO2 "global warming" scenario, with a concurrent warming of degrees centigrade degrees Fahrenheit by the year In addition it assumes that precipitation, primarily in the form of rain, will increase over the same time period about 10 percent based on the.

This equipment will outline the geological conditions under the water, which will give the scientists a better understanding of the geology and hydrology of the sandy glacial deposits underlying.

For questions about this project, please contact the speaker, John Crusius at jcrusius usgs. The northern Gulf of Alaska GoA maintains a productive ecosystem, with commercially important fisheries. A satellite image shows Ingolf Fjord, Greenland July 29, Picture taken July 29, Such events can create feedback loops that drive further warming and melting in Greenland, said Marco Tedesco, a climate scientist at Columbia University.

As snow melts, it exposes darker ice or ground beneath, which absorbs more sunlight rather than reflecting it back out of the atmosphere.

Tedesco and other scientists have warned that models used to project future ice loss do not capture the impact of changing atmospheric circulation patterns - meaning they may be underestimating the future melting of Greenland, which is located between the Arctic and Atlantic oceans.



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