词条 | Dr. Neil Trivett Global Atmosphere Watch Observatory |
释义 |
| name = Dr. Neil Trivett Global Atmosphere Watch Observatory | image = Gaw lab 20160601.jpg | caption = The observatory in June 2016 | organization = Environment and Climate Change Canada | location = Alert, Nunavut, Canada | coords = {{Coord|82|27|03|N|62|30|26|W|type:landmark|display=inline,title}} | map_type = Arctic | altitude = 185 m | established = {{Start date|1986|08|29}} | website = {{URL|https://www.ec.gc.ca/scitech/default.asp?lang=En&n=52F708A1-1|www.ec.gc.ca/}} }} The Dr. Neil Trivett Global Atmosphere Watch Observatory is an atmospheric baseline station operated by Environment and Climate Change Canada located at Alert, Nunavut, on the north-eastern tip of Ellesmere Island, about 800 km south of the geographic north pole. The observatory is the northernmost of 31 Global Stations in an international network coordinated by the World Meteorological Organization (WMO) under its Global Atmosphere Watch (GAW) program to study the long-term effects of pollution on the atmospheric environment.[1] Among these 31 stations, Alert is one of three greenhouse gas "intercomparison supersites",[2] along with Mauna Loa in Hawaii and Cape Grim in Australia, which, due to their locations far from industrial activity, provide the international scientific community with a baseline record of atmospheric chemistry. GeographyThe observatory is located on a plateau about 6 km south of Canadian Forces Station (CFS) Alert, which is itself located on the shore of the Lincoln Sea, 15 kilometres from the mouth of the Nares Strait. The region is characterized by recent glacial activity, with still extant glaciers visible among the peaks of the United States Range approximately 40 kilometres to the west. The landscape immediately surrounding the observatory is undulating, marked by cliffs and crevasses and a number of small rivers which can become impassable during freshet.[3] To the south, the Winchester Hills are the dominant visible feature. A number of small freshwater lakes provide CFS Alert (and by extension, the observatory) with drinking water. Due to its high latitude, the observatory experiences 24-hour daylight from the beginning of April to early September, and the sun remains below the horizon from mid-October to late February. The intermediate periods are marked by a slight diurnal cycle. The dark season is responsible for much of the unique atmospheric chemistry that occurs during polar sunrise. The lack of sunlight to act as a catalyst causes a buildup of pollution from industrial areas down south, and the polar vortex amplifies this effect by containing pollution within the high Arctic. During sunrise, this pollution is responsible for a phenomenon known as Arctic haze. ClimateAlert's climate is exceptionally dry, seeing very little annual precipitation. (It is, in fact, considered a desert.) What rain does fall generally comes in the form of mist or drizzle. Heavy snowfalls are typically confined to the period from September through November, but can occur again after polar sunrise. Fog is common due to proximity to the ocean, particularly in the summer and fall. When temperatures drop below freezing in September and October, the damp air also causes accumulations of hoar frost. Though conditions in Alert are cold, with only two months of the year seeing average temperatures above the freezing point (snow is possible in any month of the year), they are not as cold as other locations further south, such as Eureka, because proximity to the Arctic Ocean has as a moderating effect. It is more accurate to characterize conditions in Alert as consistently cold, rather than extremely cold. Prevailing winds at the observatory are from the southwest, which usually bring clear skies and warmer temperatures. North winds off the ocean are typically accompanied by fog and sudden drops in temperature. (North winds are also unwelcome at the observatory, as they bring exhaust from the station's diesel generators.) Conditions are typically calm through the dark winter months, once the polar vortex has set up for the season. Three out of five days have wind speeds below two metres per second at this time of year. (However, when windy conditions arise in the winter, they tend to be extreme. Storms can last for days at a time.) These conditions continue through polar sunrise, but reverse dramatically with the onset of freshet, which brings high, gusting winds. HistoryThe establishment of the Joint Arctic Weather Station (JAWS) on April 9, 1950[4] marked the beginning of continuous meteorological measurements in Alert. The weather station frequently provided support for scientific research in Alert, including the collection of weekly flask samples for the measurement of carbon dioxide, the first of which was taken on July 8, 1975.[5] Increasing interest in studies of phenomena such as Arctic haze led to a conference in 1977 in Lillestrøm, Norway with participation from scientists of seven different countries. Following this conference, the Arctic Air-Sampling Network (AASN) was created to share data between scientific organizations in each member nation.[6] To fulfill Canadian obligations to this program, the Canadian Arctic Aerosol Sampling Network (CAASN) was created, eventually consisting of three stations: Mould Bay (April 1979), Igloolik (November 1979), and Alert (July 1980).[7] In 1984, the program was condensed and refocused. The sampling programs in Igloolik and Mould Bay were discontinued, and the program in Alert became part of the core mandate of the newly reformed Canadian Arctic Aerosol Chemistry Program (CAACP).[8] The gradually increasing amount of experimental research being done in Alert made the construction of a permanent observatory a viable option. In 1985, the Canadian Baseline Program was founded, and on August 29 the following year the Alert Background Air Pollution Monitoring Network (BAPMoN) Observatory was officially opened. In 1989, the WMO's BAPMoN program was merged with the Global Ozone Observing System (GO3OS) to form the Global Atmosphere Watch Program.[9] In 1992, the original observatory building was expanded to roughly three times its size, including the addition of a 10 m tall walk-up tower. Following the death of Dr. Neil Trivett in 2002 (an Environment Canada researcher who was largely responsible for the construction of the observatory), it was officially renamed in July 2006 as the Dr. Neil Trivett Global Atmosphere Watch Observatory.[10] Measurements and researchIn addition to the ongoing flask sample programs, the observatory maintains a core group of continuous measurement programs which include monitoring of aerosols, mercury, greenhouse gases, ozone (both ground level and stratospheric), broadband solar irradiance and albedo, permafrost temperatures,[11] persistent organic pollutants (POPs), and ground level meteorological conditions.[12] The observatory also supports experimental testing of new monitoring equipment, and short-term, intensive research programs, e.g., NETCARE (Network on Climate and Aerosols: Addressing Key Uncertainties in Remote Canadian Environments).[13] Much of the research and data collection at the observatory is collaborative, including long-standing partnerships with, e.g., NOAA,[14][15] the University of Heidelberg,[16] the Scripps Institution of Oceanography,[17] CSIRO,[18] Natural Resources Canada, and Health Canada.[19] Depletion eventsWhile it had been known since 1988[20] that ground level ozone underwent periodic rapid depletions during March–June each year, it was not discovered until 1995 that atmospheric mercury behaved in a nearly identical manner. (The first continuous monitoring instruments for atmospheric mercury were installed at the observatory that year.) Until that time, it was generally agreed that elemental mercury persisted in the atmosphere for 6–12 months, which allowed it to reach remote locations such as the Arctic, far from emission sources. In the springtime, elemental mercury undergoes photochemically initiated oxidation reactions and converts to a more reactive and less stable form of mercury in the atmosphere. This was a means by which mercury could be removed from the atmosphere and deposit to the ground that was not previously known.[21] These events were later termed atmospheric mercury depletion events (AMDEs), and the underlying chemistry that connects them with the simultaneous ozone depletions has been and continues to be thoroughly researched.[22] See also
References1. ^{{cite web|title=GAW Global Stations|url=http://www.wmo.int/pages/prog/arep/gaw/GAW_Global_st.html|website=WMO Extranet|publisher=World Meteorological Organization (WMO)|accessdate=22 January 2017}} 2. ^{{cite web|title=Environment and Climate Change Canada - Climate Change - Greenhouse Gases and Aerosols|url=https://www.ec.gc.ca/sc-cs/default.asp?lang=En&n=E573D6F9-1|website=www.ec.gc.ca|accessdate=23 January 2017|language=en}} 3. ^{{cite web|title=Environment and Climate Change Canada - Climate Change - Alert Nunavut|url=https://www.ec.gc.ca/mges-ghgm/default.asp?lang=En&n=3150486A-1|website=www.ec.gc.ca|accessdate=23 January 2017|language=en}} 4. ^{{cite journal|last1=Johnson|first1=J. Peter Jr.|title=The Establishment of Alert, N.W.T., Canada|journal=Arctic|date=March 1990|volume=43|issue=1|pages=21–34|doi=10.14430/arctic1587|url=http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/view/1587|accessdate=22 January 2017}} 5. ^{{cite web|title=World Data Centre for Greenhouse Gases|url=http://ds.data.jma.go.jp/gmd/wdcgg/|website=World Data Centre for Greenhouse Gases|publisher=Japan Meteorological Agency|accessdate=22 January 2017}} 6. ^{{cite journal|last1=Rahn|first1=Kenneth A.|title=The Arctic air-sampling network in 1980|journal=Atmospheric Environment|date=January 1981|volume=15|issue=8|pages=1349–1352|doi=10.1016/0004-6981(81)90340-1|bibcode=1981AtmEn..15.1349R}} 7. ^{{cite journal|last1=Barrie|first1=L.A.|last2=Hoff|first2=R.M.|last3=Daggupaty|first3=S.M.|title=The influence of mid-latitudinal pollution sources on haze in the Canadian arctic|journal=Atmospheric Environment|date=January 1981|volume=15|issue=8|pages=1407–1419|doi=10.1016/0004-6981(81)90347-4|bibcode=1981AtmEn..15.1407B}} 8. ^{{cite web|title=Canadian Arctic Aerosol Chemistry Program (CAACP)|url=https://www.ec.gc.ca/natchem/default.asp?lang=en&n=573F3546-1|publisher=Environment and Climate Change Canada|accessdate=22 January 2017}} 9. ^{{cite web|title=Background and History|url=http://www.wmo.int/pages/prog/arep/gaw/history.html|website=WMO Extranet|publisher=World Meteorological Organization|accessdate=22 January 2017}} 10. ^{{cite news|last1=Whitnell|first1=Tim|title=Scientist honoured for work|url=http://www.thespec.com/news-story/2964713-scientist-honoured-for-work/|accessdate=22 January 2017|work=The Hamilton Spectator|publisher=Metroland Media Group|date=2006-08-20}} 11. ^{{cite journal|last1=Smith|first1=Sharon L.|last2=Burgess|first2=Margo M.|last3=Riseborough|first3=Dan|last4=Mark Nixon|first4=F.|title=Recent trends from Canadian permafrost thermal monitoring network sites|journal=Permafrost and Periglacial Processes|date=January 2005|volume=16|issue=1|pages=19–30|doi=10.1002/ppp.511}} 12. ^{{cite web|title=Alert (Canada)|url=https://gawsis.meteoswiss.ch/GAWSIS//index.html#/search/station/stationReportDetails/487|website=GAWSIS Station Information System|publisher=World Meteorological Organization|accessdate=22 January 2017}} 13. ^{{cite web|title=NETCARE Website|url=https://www.netcare-project.ca/|website=www.netcare-project.ca|publisher=NETCARE|accessdate=23 January 2017}} 14. ^{{cite web|title=BSRN Stations|url=https://www.pangaea.de/ddi?request=bsrn/BSRNEvent&format=html&title=BSRN+Stations|website=www.pangaea.de|language=en}} 15. ^{{cite web|title=ESRL/GMD Aerosols Group - Alert Station Information|url=https://esrl.noaa.gov/gmd/aero/net/alt.html|website=esrl.noaa.gov|publisher=NOAA|accessdate=23 January 2017|language=EN-US}} 16. ^{{cite web|title=Institut für Umweltphysik|url=http://www.iup.uni-heidelberg.de/institut/forschung/groups/kk/en/index_html|website=www.iup.uni-heidelberg.de}} 17. ^{{cite web|title=Scripps CO2 Program|url=http://scrippsco2.ucsd.edu/|website=scrippsco2.ucsd.edu|language=en}} 18. ^{{cite web|last1=Steele|first1=L.P.|last2=Krummel|first2=P.B.|last3=Langenfelds|first3=R.L.|title=Atmospheric Carbon Dioxide Record from Alert, NWT, Canada|url=http://cdiac.ornl.gov/trends/co2/csiro/csiro-alt.html|website=cdiac.ornl.gov|publisher=CDIAC|accessdate=23 January 2017}} 19. ^{{cite web|title=Canadian Network of Northern Research Operators » » Alert – Atmospheric Radionuclides Monitoring Station|url=http://cnnro.ca/alert-atmospheric-radionuclides-monitoring-station/|website=cnnro.ca|accessdate=23 January 2017|language=en-CA|date=2015-03-26}} 20. ^{{cite journal|last1=Barrie|first1=L. A.|last2=Bottenheim|first2=J. W.|last3=Schnell|first3=R. C.|last4=Crutzen|first4=P. J.|last5=Rasmussen|first5=R. A.|title=Ozone destruction and photochemical reactions at polar sunrise in the lower Arctic atmosphere|journal=Nature|date=14 July 1988|volume=334|issue=6178|pages=138–141|doi=10.1038/334138a0|bibcode=1988Natur.334..138B}} 21. ^{{cite journal|last1=Schroeder|first1=W. H.|display-authors=etal|title=Arctic springtime depletion of mercury|journal=Nature|date=23 July 1998|volume=394|issue=6691|pages=331–332|doi=10.1038/28530|bibcode=1998Natur.394..331S}} 22. ^{{cite journal|last1=Steffen|first1=A.|display-authors=etal|title=A synthesis of atmospheric mercury depletion event chemistry in the atmosphere and snow|journal=Atmospheric Chemistry and Physics|date=12 March 2008|volume=8|issue=6|pages=1445–1482|doi=10.5194/acp-8-1445-2008}} 5 : Geophysical observatories|Atmosphere of Earth|Meteorological data and networks|Buildings and structures in Nunavut|Government buildings completed in 1986 |
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