Senin, 30 April 2012

Global Warming

"Top climate scientist James Hansen tells the story of his involvement in the science of and debate over global climate change. In doing so he outlines the overwhelming evidence that change is happening and why that makes him deeply worried about the future." Source: TED Talks external | Discuss this at the MarineBio Blog external

Current CO2 level in the atmosphere What is Global Warming aka Climate Change?

Global warming is the increase of the average temperature in the atmosphere and oceans over time due primarily to human influences. Since the late 19th century, scientists have monitored the fluctuations in temperature and studied global warming theories and trends to determine the causes and to assess the extent to which they are due to human activity. The greenhouse effect is largely caused by human-generated carbon dioxide (CO2) and, to some extent, by increases in solar activity. The term "global warming" is used to imply a human influence while "climate change" is most often used in association with changes in climate with no easily identifiable cause, such as the processes that produced the Ice Ages external.
Current climate models external (simulations) based on estimates of increasing CO2 and, to a lesser extent, by decreasing sulfate aerosols, predict that temperatures will increase by 1.4-5.8°C (2.5-10.4°F) between 1990-2100. This is a somewhat wide range; however, it is difficult to predict CO2 emissions because of the number of variables involved. Some climate studies have shown that, even in the absence of the CO2 emission variable, global climate will increase by 0.5°C (0.9°F) over the next one hundred years due to warming caused just by the ocean. In addition, models predict that sea levels will rise by about 10 external cm over the next century.
Evidence of global warming includes decreased snowfall, rising sea levels and changes to weather trends. Precipitation levels, precipitation patterns, cloud cover, severe weather, and other elements will be impacted by the increase in greenhouse gas concentrations in the atmosphere. "Greenhouse gases" are so named because they trap radiant energy from the sun that would otherwise be radiated back into space.
The Kyoto Protocol external was developed by the United Nations Framework Convention on Climate Change (UNFCCC) external as an international agreement to reduce greenhouse gas emissions worldwide. The Protocol was entered into force in February 2005, and signed by countries committed to reducing CO2 emissions and 5 other greenhouse gases. They may also engage in emissions trading, or the purchase of credits from other countries that remain under the limits of greenhouse gas emissions. In this way, countries that may exceed the limits can still comply with the protocol. To date, 141 countries have ratified the agreement. Unfortunately, neither the United States nor Australia have been participating, which has generated speculation as to whether the Kyoto Protocol will successfully reduce greenhouse gases, even if completely implemented by all signed countries.
Global climate change has been studied on a large scale based on analyses of global temperature fluctuations over thousands of years; for example, since the last Ice Age, which occurred approximately 12,000 years ago, global temperatures have been relatively stable. Studies on a smaller scale, however, show that temperatures in the lower troposphere have increased between 0.08 and 0.22°C per decade since 1979. Still, these modern day changes are not always linear, which has created a source of debate within the scientific community and the news media.
The study of paleoclimatology external (ancient climates) is increasingly linked to modern day climate study. For example, the Earth was in an ice age for the last 160,000 years prior to the end of the last Ice Age. Earlier studies of this time period showed little variability in temperatures; however, more recent studies showed the variability to be about twice as great as previously published, indicating that temperature fluctuations are more frequent throughout time than first thought. However, this does not negate the impact of human activity on the current rate of global warming.
Climate change is caused by both natural and external forces, the latter including both human—greenhouse gases—and non-human causes such as changes in the Earth's orbit around the Sun, solar activity, and volcanic emissions. Science is increasingly pointing to human activities as the reason that global warming is accelerating.
The greenhouse gas theory external started in the 19th century when the Swedish chemist and 1903 Nobel Laureate, Svante Arrhenius, determined that increases in greenhouse gas concentration would lead to higher global mean temperatures, while decreases would lead to colder global mean temperatures. His finding was a result of his research on ice ages, and was largely rejected by his peers at the time. A colleague of Arrhenius, Arvid Högbom, was one of the first scientists to study the carbon cycle external. Arrhenius used his data to base his assessment that in 1890, emission and absorption of CO2 in the atmosphere were roughly in balance, and that burning fossil fuels would not cause problems. However, this was based solely on the use of coal, not on the use of fossil fuels in the automobile and other industries.
Opponents to the global warming theory postulate that water vapor and clouds will cancel out warming effect of CO2 emissions. However, the warming trends over the past few decades are increasingly negating the cancellation hypothesis. Furthermore, sophisticated computer models of the climate, validated by the scientific community in demonstrating accurate simulations of known climate variations such as El Niño events external, have predicted that adding CO2 to the atmosphere will create a warmer climate in the future. The degree to which this warming will occur varies by model, however, and opponents of the global warming theory point out variables that models are not equipped to factor, such as changes in vegetation and cloud cover.
» The Biggest Control Knob: Carbon Dioxide in Earth's Climate History, Richard B. Alley, Ph.D., Penn State, American Geophysical Union (AGU) lecture, December, 2009. external
In spite of the dying debate, it is known that coal-burning power plants, automobile exhausts, factory smokestacks, and other waste vents contribute about 22 billion tons of CO2 (6 billion tons of pure carbon) and other greenhouse gases into the earth's atmosphere each year. CO2 levels have increased by about 31% since 1750, about 75% of which can be attributed to fossil fuel burning. The remaining 25% is largely due to land-use change, particularly deforestation.
In their 2006 report, the IPCC external stated that the atmospheric concentration of CO2 has exceeded levels over the natural range for the last 650,000 years. The consensus is that human activity is, in almost all aspects of global warming, the most likely cause. This is a change from the previous report that stated human activity was merely a likely cause.

Minggu, 22 April 2012

Daftar Universitas kelautan di dunia.


Marine Biology Laboratories, Institutes & Graduate Programs

Join the MarineBio Conservation SocietyThe study of marine biology often requires hands on work in a laboratory setting. There are many marine labs in the US and around the globe with a variety of research topics and resources. Some are afflilated with one or more universities, and some are departments within a university. Contact us if you have any comments, changes or additions.

« Education & Careers Resources

US West Coast

Blakely Island Field Station, Washington external
Bodega Marine Laboratory external
Friday Harbor Laboratories external
Hatfield Marine Science Center, Newport Oregon external
Hawai'i Institute of Marine Biology external
Hawai'i Undersea Research Laboratory (HURL) external
Hopkins Marine Station - Stanford University external
Long Marine Lab (of UC Santa Cruz) external
Marine Science Institute (USCB) external
Moss Landing Marine Labs external
Monterey Bay Aquarium Research Institute (MBARI) external
NMFS Southwest Fisheries Science Center Santa Cruz Lab external
Oceanic Institute (Hawai'i Pacific University affiliate) external
Oregon Institute of Marine Biology external
Pacific Marine Environmental Laboratory external
Romberg-Tiburon Lab of SF State University external
School of Ocean & Earth Science & Technology Hawaii external
Scripps Institution of Oceanography external
Shannon Point Marine Center, W. Washington State external
University of Washington - College of Ocean and Fishery Science external
West Coast & Polar Regions Undersea Research Center external
Wrigley Institute of Environmental Studies, Univ. of Southern California external
Scripps Institute of Oceanography

US East Coast

Atlantic Oceanographic and Meteorological Laboratory (AOML) external
Belle W. Baruch Institute for Marine & Coastal Science, University of South Carolina external
Bigelow Laboratory for Ocean Sciences, Maine external
Center for Marine Science and Technology North Carolina external
Chesapeake Biological Lab, University of Maryland external
Darling Marine Center, University of Maine external
Duke University Marine Laboratory external
Five Colleges Coastal and Marine Science Program - Amherst MA region external
Florida State University, Edward Ball Marine Laboratory external
Grice Marine Biological Laboratory, College of Charleston, SC external
Harbor Branch Oceanographic Institution external
Horn Point Laboratory, University of Maryland external
Marine Institute University of Georgia external
Marine Sciences Program at Avery Point - University of Connecticut external
Marine Sciences Program, University of North Carolina: Chapel Hill external
Medical University of South Carolina - Marine Biomedicine and Env. Sci. external
Mid-Atlantic Bight (MAB) National Undersea Research Center external
Mt. Desert Island Biological Lab, Maine external
National Undersea Research Center for the North Atlantic and Great Lakes (NURC-NA&GL) external
NOAA's Undersea Research Center at UNCW external
Pew Institute for Ocean Science external
Pew Institute for Ocean Science Pew Fellowships Program external
Rhode Island, Graduate School of Oceanography external
Rutgers University, Institute of Marine and Coastal Sciences external
Skidaway Institute of Oceanography external
Shoals Marine Laboratory external
South Carolina - Belle W. Baruch Institute for Marine Biology and Coastal Research external
Stony Brook, Marine Sciences Research Center external
University of South Florida - College of Marine Science external
University of Maine - School of Marine Sciences external
University of Maryland - MEES Graduate Program external
University of South Carolina - Marine Science Graduate Program external
Virginia Institute of Marine Science external
Whitney Laboratory for Marine Bioscience, University of Florida external
Woods Hole Marine Biology Laboratory external
Woods Hole Oceanographic Institution external
Woods Hole Sea Education Association external

US Gulf Coast & the Caribbean

Outside of the US

Alfred Wegener Institute for Polar and Marine Research (AWI), Germany external
Australian Antarctic Division external
Bermuda Biological Station for Research external
Cawthron Institute of New Zealand - Specializing in Aquaculture external
CSIRO Marine Research - Australia external
Dept. of Fisheries and Marine Biology, Univ. of Bergen, Norway external
Dominica - Institute of Tropical Marine Ecology external
Discovery Bay Marine Laboratory, Jamaica, West Indies external
Hofstra University Marine Lab, Jamaica, West Indies external
Huntsman Marine Lab, St. Andrews, New Brunswick, Canada external
IAEA Marine Environmental Studies Laboratory (MESL), Monaco external
Kristineberg Marine Research Station, Sweden external
Max Planck Institute for Marine Microbiology, Bremen, Germany external
Memorial University of Newfoundland, Ocean Sciences Centre, Canada external
Millport - University Marine Biological Station, Scotland external
NIWA (National Institute of Water and Atmospheric Research), New Zealand external
Observatoire Oceanologique de Banyuls-sur-Mer, France external
Observatoire Oceanologique de Villefranche-sur-Mer, France external
Plymouth Marine Laboratory, UK external
SAMS, Scottish Association for Marine Science - Dunstaffnage Marine Laboratory external
Station Biologique de Roscoff, France external
Tjärnö Marine Biological Laboratory, Sweden external
Unis: Norwegian University Consortium on Svalbard in the Arctic external
University of Copenhagen Marine Biological Laboratory external
Research - Marine Science and Technology - University of Newcastle, UK external
University of Wales, Bangor, School of Ocean Sciences external