![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
![]() |
. | ![]() |
. |
![]()
This year's seasonal ozone hole over Antarctica was the third largest on record, but forecasters are uncertain how it will behave in the future, the World Meteorological Organisation (WMO) said Tuesday. The hole peaked last month at almost 27 million square kilometers), and then began shrinking as usual, the WMO said in a statement. That was just short of the record 28 million square kilometers) set in 2003, the WMO said. The second-largest hole was logged in 2000. "Because of uncertainties linked to climate change, we don't know if we reached the biggest ozone hole ever in 2003 or if it will be bigger sometime in the future," said WMO ozone expert Geir Braathen. "But it's not likely that it will get much bigger. It seems like we have reached a plateau." "The question is how long it will take before we get back to pre-ozone hole levels," he told reporters. The hole in the ozone layer, discovered in the 1980s, is created by atmospheric conditions and pollution, and fluctuates according to season and prevailing weather. Ozone, a molecule of oxygen, is a stratospheric shield for life on Earth, filtering out dangerous ultraviolet rays from the Sun that damage vegetation and can cause skin cancer and cataracts. The protective layer has been increasingly damaged by man-made chemicals, especially bromine, chlorine and chlorofluorocarbons (CFCs). CFCs are an aerosol gas, previously used in refrigerators, whose use was belatedly controlled by an international treaty, the Montreal Protocol signed on September 16, 1987. "As the amount of chlorine and bromine will continue to decline over the next decade -- very slowly -- one expects the ozone whole to get smaller and smaller," Braathen said. "But at the same time there is also this issue of climate change, which leads to high temperatures on the ground while in the stratosphere temperatures will decrease. And that will encourage more ozone loss in the Arctic and Antarctic." "This is an open question. We don't know what the effect will be." All rights reserved. � 2005 Agence France-Presse. Sections of the information displayed on this page (dispatches, photographs, logos) are protected by intellectual property rights owned by Agence France-Presse. As a consequence, you may not copy, reproduce, modify, transmit, publish, display or in any way commercially exploit any of the content of this section without the prior written consent of Agence France-Presse. Related Links TerraDaily Search TerraDaily Subscribe To TerraDaily Express ![]() ![]() A new global study involving long-term data from satellites and ground stations indicates Earth's ozone layer, while still severely depleted following decades of thinning from industrial chemicals in the atmosphere, is no longer in decline.
|
![]() |
|
The content herein, unless otherwise known to be public domain, are Copyright 1995-2016 - Space Media Network. All websites are published in Australia and are solely subject to Australian law and governed by Fair Use principals for news reporting and research purposes. AFP, UPI and IANS news wire stories are copyright Agence France-Presse, United Press International and Indo-Asia News Service. ESA news reports are copyright European Space Agency. All NASA sourced material is public domain. Additional copyrights may apply in whole or part to other bona fide parties. Advertising does not imply endorsement, agreement or approval of any opinions, statements or information provided by Space Media Network on any Web page published or hosted by Space Media Network. Privacy Statement All images and articles appearing on Space Media Network have been edited or digitally altered in some way. Any requests to remove copyright material will be acted upon in a timely and appropriate manner. Any attempt to extort money from Space Media Network will be ignored and reported to Australian Law Enforcement Agencies as a potential case of financial fraud involving the use of a telephonic carriage device or postal service. |