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| Station Characteristics | 2008-03-12/184 |
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| GAW ID | BRW | Barrow (AK) (United States) |
| WMO ID | Global station in WMO RA IV - North/Central America | |
| station status | established 1973 / full operation | 71.32301°N 156.61147°W (11 m a.s.l.) |
| time zone | UTC-9 | http://www.esrl.noaa.gov/gmd/obop/brw/ |
| climate zone | ET (Tundra climate) | |
| other affiliations | AERONET(Barrow), BSRN, NOAA-ESRL/CCG, NOAA-ESRL/AERO(BRW), NDACC |
| description | Barrow Observatory, established in 1973, is located near sea level 8 km east of Barrow, Alaska at 71.32 degrees north. This facility is manned year around by 2 engineers/scientists who often commute to work in winter on snow machines. Due to its unique location, dedicated and highly trained staff, excellent power and communications infrastructure, the Barrow Observatory is host to numerous cooperative research projects from around the world. BRW is located so that it receives minimal influence from anthropogenic effects. It is about 8 km northeast of the village of Barrow and has a prevailing east-northeast wind off the Beaufort Sea. It is attended at least 5 days a week for routine inspection and maintenance of the instrumentation. In addition, the National Weather Service (NWS) maintains a weather observing facility in Barrow. Although the measurements at Barrow are made over open tundra, there are large lagoons and a number of lakes in the vicinity, and the Arctic Ocean is less than 3 km northwest of the site. Because of its proximity to these bodies of water and the fact that the prevailing winds are off the Beaufort Sea, BRW is perhaps best characterized as having an Arctic maritime climate affected by variations of weather and sea ice conditions in the Central Arctic. |
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| References |
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| Stone, R. S., et al. (2008), Radiative impact of boreal smoke in the Arctic: Observed and modeled, Journal of Geophysical Research-Atmospheres, 113 | ||
| Zellweger, Christoph, et al. (2008), System and Performance Audit of Surface Ozone,Carbon Monoxide, Methane and Nitrous Oxide at the Global GAW Station Barrow, USA, March 2008, WCC-Empa Report 08/1, http://gaw.empa.ch/audits/BRW_2008.pdf | ||
| Quinn, P. K., et al. (2007), Arctic haze: current trends and knowledge gaps, Tellus Series B-Chemical and Physical Meteorology, 59, 99-114 | ||
| Stone, R. S., et al. (2007), Incursions and radiative impact of Asian dust in northern Alaska, Geophysical Research Letters, 34 | ||
| Tomasi, C., et al. (2007), Aerosols in polar regions: A historical overview based on optical depth and in situ observations, Journal of Geophysical Research-Atmospheres, 112 | ||
| Sharma, S., et al. (2006), Variations and sources of the equivalent black carbon in the high Arctic revealed by long-term observations at Alert and Barrow: 1989-2003, Journal of Geophysical Research-Atmospheres, 111 | ||
| Stohl, A., et al. (2006), Pan-Arctic enhancements of light absorbing aerosol concentrations due to North American boreal forest fires during summer 2004, Journal of Geophysical Research-Atmospheres, 111 | ||
| Delene, D. J. and Ogren, J. A. (2002), Variability of aerosol optical properties at four North American surface monitoring sites, Journal of the Atmospheric Sciences, 59, 1135-1150 | ||
| Quinn, P. K., et al. (2002), A 3-year record of simultaneously measured aerosol chemical and optical properties at Barrow, Alaska, Journal of Geophysical Research-Atmospheres, 107 | ||
| Bodhaine, B.A. (1995), Aerosol absorption measurements at Barrow, Mauna Loa and the South Pole, J. Geophys. Res, 100, 8967--8975 | ||
| Anderson, BE, et al. (1994), Partial Bibliography: National Oceanic and Atmospheric Administration (NOAA) Climate Monitoring and Diagnostics Laboratory (CMDL), Barrow Observatory Compiled by Dan Endres, NOAA/CMDL, November 1998, Geophys. Res. Lett, 21, 433--436, www.arcus.org/Logistics/barrow/cmdl_bib.pdf | ||
| DUTTON, EG, et al. (1985), Solar radiation at the Barrow, Alaska, GMCC (Geophysical Monitoring for Climatic Change) Baseline Observatory, 1976-1983, Unknown, , adsabs.harvard.edu/abs/1985STIN...8624646D | ||
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