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On the predominance of unstable atmospheric conditions in the marine boundary layer offshore of the U.S. northeastern coast
Author(s) -
Archer Cristina L.,
Colle Brian A.,
Veron Dana L.,
Veron Fabrice,
Sienkiewicz Matthew J.
Publication year - 2016
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2016jd024896
Subject(s) - offshore wind power , turbulence kinetic energy , wind speed , atmospheric instability , environmental science , planetary boundary layer , wind profile power law , submarine pipeline , wind stress , meteorology , context (archaeology) , boundary layer , maximum sustained wind , wind gradient , wind direction , atmospheric sciences , wind shear , wind power , geology , turbulence , geography , oceanography , physics , engineering , paleontology , electrical engineering , thermodynamics
The marine boundary layer of the northeastern U.S. is studied with focus on wind speed, atmospheric stability, and turbulent kinetic energy (TKE), the three most relevant properties in the context of offshore wind power development. Two long‐term observational data sets are analyzed. The first one consists of multilevel meteorological variables measured up to 60 m during 2003–2011 at the offshore Cape Wind tower, located near the center of the Nantucket Sound. The second data set comes from the 2013–2014 IMPOWR campaign (Improving the Modeling and Prediction of Offshore Wind Resources), in which wind and wave data were collected with new instruments on the Cape Wind platform, in addition to meteorological data measured during 19 flight missions offshore of New York, Connecticut, Rhode Island, and Massachusetts. It is found that, in this region: (1) the offshore wind resource is remarkable, with monthly average wind speeds at 60 m exceeding 7 m s −1 all year round, highest winds in winter (10.1 m s −1 ) and lowest in summer (7.1 m s −1 ), and a distinct diurnal modulation, especially in summer; (2) the marine boundary layer is predominantly unstable (61% unstable vs. 21% neutral vs. 18% stable), meaning that mixing is strong, heat fluxes are positive, and the wind speed profile is often nonlogarithmic (~40% of the time); and (3) the shape of the wind speed profile (log versus nonlog) is an effective qualitative proxy for atmospheric stability, whereas TKE alone is not.