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Barrow Urban Heat Island Study


 

 

 


The PowerPoint presentation was delivered at the Annual Conference of the Association of American Geographers in New Orleans in March 2003.

The pdf file is a an article published in the International Journal of Climatology in 2003.  The Abstract is given below.

ABSTRACT

The village of Barrow, Alaska is the northernmost settlement in the United States and the largest native community in the Arctic.  The population has grown from about 300 residents in 1900 to more than 4600 in 2000.  In recent decades, a general increase of mean annual and mean winter air temperature has been recorded near the center of the village, and a concurrent trend of progressively earlier snowmelt in the village has been documented.  Satellite observations and data from a nearby climate observatory indicate a corresponding but much weaker snowmelt trend in the surrounding regions of relatively undisturbed tundra.  Because the region is underlain by ice-rich permafrost, there is concern that early snowmelt will increase the thickness of the thawed layer in summer and threaten the structural stability of roads, buildings, and pipelines.  Here we demonstrate the existence of a strong urban heat island (UHI) during winter.  Fifty-four data loggers were installed in the ~150 km2 study area to monitor hourly air and soil temperature, and daily spatial averages were calculated using the 6-7 warmest and coldest sites.  During winter (December 2001-March 2002), the urban area averaged 2.2° C warmer than the hinterland.  The strength of the UHI increased as wind velocity decreased, reaching an average value of 3.2° C under calm (< 2 m s-1) conditions and maximum single-day magnitude of 6° C.  UHI magnitude generally increased with decreasing air temperature in winter, reflecting the input of anthropogenic heat to maintain interior building temperatures.  On a daily basis, the UHI reached its peak intensity in the late evening and early morning.  There was a strong positive relation between monthly UHI magnitude and natural gas production/use.  Integrated over the period September-May, there was a 9% reduction in accumulated freezing degree days in the urban area.  The evidence suggests that urbanization has contributed to early snowmelt in the village.

 The following article is also available as a pdf file; it describes the summer temperature fields around Barrow.

The Urban Heat Island in Winter at Barrow, Alaska.. Article published in International Journal of Climatology 23, 1889-1905, 2003.

The Summer Climate of an Arctic Coastal Village: Preliminary Observations From the Barrow Urban Heat-Island Study. Article published in Polar Geography, 27(3), 2003.

Hinkel presentation in Sweden, June 2006 .

Anthropogenic Heat Island at Barrow, Alaska, During Winter: 2001-2005. Article published in Journal of Geophysical Research, Vol. 112, D06118, doi:10.1029/2006JD007837, 2007.

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For further information, please contact

Dr. Kenneth M. Hinkel, Department of Geography, 400F Braunstein, ML 131, University of Cincinnati, Cincinnati, Ohio 45221-0131
Phone: (513) 556-3430, Fax: (513) 556-3370, Kenneth.Hinkel@uc.edu