Mostrando entradas con la etiqueta The Ozone Hole. Mostrar todas las entradas
Mostrando entradas con la etiqueta The Ozone Hole. Mostrar todas las entradas

viernes, 22 de agosto de 2014

NASA : Ozone-Depleting Compound Persists, NASA Research Shows


Satellites observed the largest ozone hole over Antarctica in 2006. Purple and blue represent areas of low ozone concentrations in the atmosphere; yellow and red are areas of higher concentrations.
Satellites observed the largest ozone hole over Antarctica in 2006. Purple and blue represent areas of low ozone concentrations in the atmosphere; yellow and red are areas of higher concentrations.
Image Credit: 
NASA
 
NASA research shows Earth's atmosphere contains an unexpectedly large amount of an ozone-depleting compound from an unknown source decades after the compound was banned worldwide.

Carbon tetrachloride (CCl4), which was once used in applications such as dry cleaning and as a fire-extinguishing agent, was regulated in 1987 under the Montreal Protocol along with other chlorofluorocarbons that destroy ozone and contribute to the ozone hole over Antarctica. Parties to the Montreal Protocol reported zero new CCl4 emissions between 2007-2012.
However, the new research shows worldwide emissions of CCl4 average 39 kilotons per year, approximately 30 percent of peak emissions prior to the international treaty going into effect.
"We are not supposed to be seeing this at all," said Qing Liang, an atmospheric scientist at NASA's Goddard Space Flight Center in Greenbelt, Maryland, and lead author of the study. "It is now apparent there are either unidentified industrial leakages, large emissions from contaminated sites, or unknown CCl4 sources."

Youtube Override: 
NASA video discusses new research that shows Earth's atmosphere contains an unexpectedly large amount of an ozone-depleting compound from an unknown source decades after the compound was banned worldwide.
 
As of 2008, CCl4 accounted for about 11 percent of chlorine available for ozone depletion, which is not enough to alter the decreasing trend of ozone-depleting substances. Still, scientists and regulators want to know the source of the unexplained emissions.

For almost a decade, scientists have debated why the observed levels of CCl4 in the atmosphere have declined slower than expectations, which are based on what is known about how the compound is destroyed by solar radiation and other natural processes.
"Is there a physical CCl4 loss process we don't understand, or are there emission sources that go unreported or are not identified?" Liang said.
With zero CCl4 emissions reported between 2007-2012, atmospheric concentrations of the compound should have declined at an expected rate of 4 percent per year. Observations from the ground showed atmospheric concentrations were only declining by 1 percent per year.
To investigate the discrepancy, Liang and colleagues used NASA's 3-D GEOS Chemistry Climate Model and data from global networks of ground-based observations. The CCl4 measurements used in the study were made by scientists at the National Oceanic and Atmospheric Administration's (NOAA's) Earth System Research Laboratory and NOAA's Cooperative Institute for Research in Environmental Sciences at the University of Colorado, Boulder.
Model simulations of global atmospheric chemistry and the losses of CCl4 due to interactions with soil and the oceans pointed to an unidentified ongoing current source of CCl4. The results produced the first quantitative estimate of average global CCl4 emissions from 2000-2012.
In addition to unexplained sources of CCl4, the model results showed the chemical stays in the atmosphere 40 percent longer than previously thought. The research was published online in the Aug. 18 issue of Geophysical Research Letters.
"People believe the emissions of ozone-depleting substances have stopped because of the Montreal Protocol," said Paul Newman, chief scientist for atmospheres at NASA's Goddard Space Flight Center, and a co-author of the study. "Unfortunately, there is still a major source of CCl4 out in the world."
NASA monitors Earth's vital signs from land, air and space with a fleet of satellites and ambitious airborne and ground-based observation campaigns. NASA develops new ways to observe and study Earth's interconnected natural systems with long-term data records and computer analysis tools to better see how our planet is changing. The agency shares this unique knowledge with the global community and works with institutions in the United States and around the world that contribute to understanding and protecting our home planet.
For more information about NASA's Earth science activities in 2014, visit:
For information on the Antarctic ozone hole, visit:

NASA
Guillermo Gonzalo Sánchez Achutegui
ayabaca@gmail.com
ayabaca@hotmail.com
ayabaca@yahoo.com
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domingo, 8 de septiembre de 2013

nsf.gov - News - NSF Frontiers in Earth-System Dynamics awards explore links among Earth processes and systems

Scientists investigate a changing planet now and in the past, with a view toward predicting its future,.
graphic illustration showing a termometer, the sun, ocean and ice
From burning hot to freezing cold places, FESD awardees conduct research on Earth systems.
Credit and Larger Version
September 4, 2013
The effects of the ozone hole on the Southern Hemisphere's climate; biodiversity in the Amazon/Andean forest; Earth system dynamics and human evolution in Africa; deep-Earth dynamics and long-term climate; the Earth system and its oxygen; and links among volcanoes, oceans, ice and carbon.
To explore the connections among our planet's dynamic systems, the National Science Foundation (NSF) has made awards totaling $28 million for research on these six topics. They are the second set of grants in NSF's Frontiers in Earth-System Dynamics (FESD) Program. Earth is often characterized as "dynamic" because its systems are variable over time and can respond rapidly to changes.
The FESD Program is supported by three divisions in NSF's Directorate for Geosciences (GEO): Atmospheric and Geospace Sciences, Earth Sciences and Ocean Sciences.
"FESD is one of GEO's efforts to fund high-risk, high-return research," says Roger Wakimoto, NSF Assistant Director for Geosciences.
"The awards reflect a multi-disciplinary approach that goes beyond what a single core program can support," says Wakimoto. "The 2013 awardees' projects are impressive, and will lead to exciting research discoveries."
The goals of the FESD program are to foster an interdisciplinary and multi-scale understanding of the interplay among and within the sub-systems at work on Earth, and to catalyze research in geoscience areas poised for major advances.
The program also seeks to improve data resolution and modeling capabilities to more realistically simulate complex processes and forecast disruptive or threshold events, and to improve knowledge of the resilience of the Earth and its systems.
Understanding and predicting the behavior of the complex and evolving Earth system was identified as a major challenge in the report GEOVision: Unraveling Earth's Complexities Through the Geosciences, released by the NSF Advisory Committee for Geosciences.
"Earth's systems interact with each other on different scales, linked across space and time," states the GEOVision report. "Changes in one component affect the status and function of other elements, and not always in straightforward or obvious ways."
Studying one component in isolation yields an incomplete, and sometimes misleading, picture, according to the report.
"One of the most striking characteristics of the Earth system is the presence of patterns," states GEOVision.
"Understanding how such methodical arrangements emerge over Earth's history may provide an important key to predicting Earth-system behavior."
The FESD awards address the need to discover and predict rates of change in these systems by fostering an integrated and multi-scale understanding of Earth's processes and systems, improving data resolution and modeling capabilities to discover and predict how rapidly these processes and systems are changing, and determining how resilient they are to the effects of human activities.
The recent human footprint on Earth has been large. The FESD awards will help scientists discover how large, as measured against naturally-occurring events; how Earth might respond; and what actions might be taken now and in the future to help shrink our global footprint.
2013 NSF FESD Awards
 Ariel Anbar, Arizona State University
 Paul Baker, Duke University
 Andrew Cohen, University of Arizona
Charles Langmuir, Harvard University
Cin-Ty Lee, William Marsh Rice University
John Marshall, Massachusetts Institute of Technology
-NSF-
Media Contacts Cheryl Dybas, NSF (703) 292-7734 cdybas@nsf.gov
Related WebsitesNSF News: NSF Advisory Committee Offers New View for the Geosciences:
http://www.nsf.gov/geo/acgeo/geovision/start.jsp
NSF News: First Awards Made in Frontiers in Earth-System Dynamics Program:
The National Science Foundation (NSF) is an independent federal agency that supports fundamental research and education across all fields of science and engineering. In fiscal year (FY) 2012, its budget was $7.0 billion. NSF funds reach all 50 states through grants to nearly 2,000 colleges, universities and other institutions. Each year, NSF receives about 50,000 competitive requests for funding, and makes about 11,500 new funding awards. NSF also awards about $593 million in professional and service contracts yearly.
Useful NSF Web Sites:
NSF Home Page:
 http://www.nsf.gov/news/
For the News Media:
http://www.nsf.gov/news/newsroom.jsp
Science and Engineering Statistics:
Volcanic erruption
Volcanoes, ice, oceans and carbon: Their connections are the subject of FESD research.
Credit and Larger Version
photo of forest and mountains in the Andes region
Scientists funded by the FESD Program are studying Andes and Amazon biodiversity.
Credit and Larger Version
Photo of iron formations in soil in a canyon
Banded iron formations: important in the development of Earth's oxygenated environment.
Credit and Larger Version
Lake Turkana and vehicles on it banks in Kenya
Deposits in Kenya's Lake Turkana help scientists link paleoclimate and human evolution.
Credit and Larger Version
Illustration showing the ozone hole in the Southern Hemisphere
FESD grantees are studying the ozone hole and its effects on Southern Hemisphere climate.
Credit and Larger Version
 
The National Science Foundation (NSF)
Guillermo Gonzalo Sánchez Achutegui

domingo, 28 de octubre de 2012

NASA - 2012 Antarctic Ozone Hole Second Smallest in 20 Years

 
 False-color view of total ozone over the Antarctic pole. The purple and blue colors are where there is the least ozone, and the yellows and reds are where there is more ozone.

October 2012 (All images)
 October Climatology (All images)
 http://ozonewatch.gsfc.nasa.gov/

Ozone facts

What is ozone?

Ozone is a colorless gas. Chemically, ozone is very active; it reacts readily with a great many other substances. Near the Earth’s surface, those reactions cause rubber to crack, hurt plant life, and damage people’s lung tissues. But ozone also absorbs harmful components of sunlight, known as “ultraviolet B”, or “UV-B”. High above the surface, above even the weather systems, a tenuous layer of ozone gas absorbs UV-B, protecting living things below.

What is a Dobson Unit?

The Dobson Unit (DU) is the unit of measure for total ozone. If you were to take all the ozone in a column of air stretching from the surface of the earth to space, and bring all that ozone to standard temperature (0 °Celsius) and pressure (1013.25 millibars, or one atmosphere, or “atm”), the column would be about 0.3 centimeters thick. Thus, the total ozone would be 0.3 atm-cm. To make the units easier to work with, the “Dobson Unit” is defined to be 0.001 atm-cm. Our 0.3 atm-cm would be 300 DU.

What is the ozone hole?

Each year for the past few decades during the Southern Hemisphere spring, chemical reactions involving chlorine and bromine cause ozone in the southern polar region to be destroyed rapidly and severely. This depleted region is known as the “ozone hole”.
The area of the ozone hole is determined from a map of total column ozone. It is calculated from the area on the Earth that is enclosed by a line with a constant value of 220 Dobson Units. The value of 220 Dobson Units is chosen since total ozone values of less than 220 Dobson Units were not found in the historic observations over Antarctica prior to 1979. Also, from direct measurements over Antarctica, a column ozone level of less than 220 Dobson Units is a result of the ozone loss from chlorine and bromine compounds. 

2012 Antarctic Ozone Hole Second Smallest in 20 Years
 
 
WASHINGTON -- The average area covered by the Antarctic ozone hole this year was the second smallest in the last 20 years, according to data from NASA and National Oceanic and Atmospheric Administration (NOAA) satellites. Scientists attribute the change to warmer temperatures in the Antarctic lower stratosphere.

The ozone hole reached its maximum size Sept. 22, covering 8.2 million square miles (21.2 million square kilometers), or the area of the United States, Canada and Mexico combined. The average size of the 2012 ozone hole was 6.9 million square miles (17.9 million square kilometers). The Sept. 6, 2000 ozone hole was the largest on record at 11.5 million square miles (29.9 million square kilometers).

"The ozone hole mainly is caused by chlorine from human-produced chemicals, and these chlorine levels are still sizable in the Antarctic stratosphere," said NASA atmospheric scientist Paul Newman of NASA's Goddard Space Flight Center in Greenbelt, Md. "Natural fluctuations in weather patterns resulted in warmer stratospheric temperatures this year. These temperatures led to a smaller ozone hole."

The ozone layer acts as Earth's natural shield against ultraviolet radiation, which can cause skin cancer. The ozone hole phenomenon began making a yearly appearance in the early 1980s. The Antarctic ozone layer likely will not return to its early 1980s state until about 2065, Newman said. The lengthy recovery is because of the long lifetimes of ozone-depleting substances in the atmosphere. Overall atmospheric ozone no longer is declining as concentrations of ozone-depleting substances decrease. The decrease is the result of an international agreement regulating the production of certain chemicals.

This year also showed a change in the concentration of ozone over the Antarctic. The minimum value of total ozone in the ozone hole was the second highest level in two decades. Total ozone, measured in Dobson units (DU), reached 124 DU on Oct. 1. NOAA ground-based measurements at the South Pole recorded 136 DU on Oct. 5. When the ozone hole is not present, total ozone typically ranges from 240-500 DU.

This is the first year growth of the ozone hole has been observed by an ozone-monitoring instrument on the Suomi National Polar-orbiting Partnership (NPP) satellite. The instrument, called the Ozone Mapping Profiler Suite (OMPS), is based on previous instruments, such as the Total Ozone Mapping Spectrometer (TOMS) and the Solar Backscatter Ultraviolet instrument (SBUV/2), which have flown on multiple satellites. OMPS continues a satellite record dating back to the early 1970s.

In addition to observing the annual formation and extent of the ozone hole, scientists hope OMPS will help them better understand ozone destruction in the middle and upper stratosphere with its Nadir Profiler. Ozone variations in the lower stratosphere will be measured with its Limb Profiler.

"OMPS Limb looks sideways, and it can measure ozone as a function of height," said Pawan K. Bhartia, a NASA atmospheric physicist and OMPS Limb instrument lead. "This OMPS instrument allows us to more closely see the vertical development of Antarctic ozone depletion in the lower stratosphere where the ozone hole occurs."

NASA and NOAA have been monitoring the ozone layer on the ground and with a variety of instruments on satellites and balloons since the 1970s. Long-term ozone monitoring instruments have included TOMS, SBUV/2, Stratospheric Aerosol and Gas Experiment series of instruments, the Microwave Limb Sounder, the Ozone Monitoring Instrument, and the OMPS instrument on Suomi NPP. Suomi NPP is a bridging mission leading to the next-generation polar-orbiting environmental satellites called the Joint Polar Satellite System, which will extend ozone monitoring into the 2030s.

NASA and NOAA have a mandate under the Clean Air Act to monitor ozone-depleting gases and stratospheric depletion of ozone. NOAA complies with this mandate by monitoring ozone via ground and satellite measurements. The NOAA Earth System Research Laboratory in Boulder, Colo., performs the ground-based monitoring. The Climate Prediction Center performs the satellite monitoring.

To monitor the state of the ozone layer above Antarctica, visit:
 NASA
Guillermo GOnzalo Sánchez Achutegui
ayabaca@gmail.com
ayabaca@hotmail.com
ayabaca@yahoo.com
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