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Wind Climatology of the Mount Washin...

Cronin, Kevin Patrick.

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Wind Climatology of the Mount Washington Observatory (1935-2013).

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Wind Climatology of the Mount Washington Observatory (1935-2013)./
作者:	Cronin, Kevin Patrick.
面頁冊數:	94 p.
附註:	Source: Masters Abstracts International, Volume: 55-02.
Contained By:	Masters Abstracts International55-02(E).
標題:	Meteorology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1602705
ISBN:	9781339185378

Wind Climatology of the Mount Washington Observatory (1935-2013).
Cronin, Kevin Patrick.

Wind Climatology of the Mount Washington Observatory (1935-2013). - 94 p.

Source: Masters Abstracts International, Volume: 55-02.

Thesis (M.S.)--Plymouth State University, 2015.

The Mount Washington Observatory (MWO), which is located on the summit of Mount Washington, New Hampshire (44.27° N, 71.30° W, 1917 m ASL), has operated and maintained more than 80 years of continuous weather observations. This is the first climatological analysis of the digitized MWO wind record (1935-present) and incorporates data from 1935-2013. The MWO station site changes and obstructions on the summit made a measurable impact on the wind record. This study did not account for the site changes or obstructions on the summit and did not attempt to make corrections on the record. Since the anemometer moved in 1980 to the current location on the Sherman Adams Building, it has been fully exposed to the prevailing westerly wind direction.

ISBN: 9781339185378Subjects--Topical Terms:

542822
Meteorology.

Wind Climatology of the Mount Washington Observatory (1935-2013).
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245 1 0 $a Wind Climatology of the Mount Washington Observatory (1935-2013).
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500 $a Source: Masters Abstracts International, Volume: 55-02.
500 $a Adviser: Eric Kelsey.
502 $a Thesis (M.S.)--Plymouth State University, 2015.
520 $a The Mount Washington Observatory (MWO), which is located on the summit of Mount Washington, New Hampshire (44.27° N, 71.30° W, 1917 m ASL), has operated and maintained more than 80 years of continuous weather observations. This is the first climatological analysis of the digitized MWO wind record (1935-present) and incorporates data from 1935-2013. The MWO station site changes and obstructions on the summit made a measurable impact on the wind record. This study did not account for the site changes or obstructions on the summit and did not attempt to make corrections on the record. Since the anemometer moved in 1980 to the current location on the Sherman Adams Building, it has been fully exposed to the prevailing westerly wind direction.
520 $a Wind speed and directional diel patterns exist during all seasons with the most consistent diel pattern seen in the summer. Summer wind speed peaks before sunrise and decrease to a minimum in the early afternoon indicating frequent planetary boundary layer exposure. The weak winter diel wind cycle implies regular exposure to the free troposphere in the winter where synoptic scale patterns dominate wind variability. The influence of large-scale atmospheric circulation patterns (e.g., Arctic Oscillation) on xiv Mount Washington wind speed is strongest during the cold season, but is relatively weak. A Theil-Sen's slope trend analysis of the Mount Washington wind record from 1981- 2013 reveals a decrease of 0.25 m s-1 decade-1. Although the finding is not statistically significant, it is consistent with similar decreasing trends observed at other Northern Hemisphere mid-latitude stations that may be a result of Arctic amplification.
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