Overlap between the Mid-Atlantic Bight Cold Pool and offshore wind lease areas

被引:1
|
作者
Horwitz, Rebecca [1 ]
Miles, Travis N. [1 ]
Munroe, Daphne [1 ,2 ]
Kohut, Josh [1 ]
机构
[1] Rutgers State Univ, Dept Marine & Coastal Sci, Ctr Ocean Observing Leadership, 71 Dudley Rd, New Brunswick, NJ 08901 USA
[2] Rutgers State Univ, Haskin Shellfish Res Lab, 6959 Miller Ave, Port Norris, NJ 08349 USA
基金
美国国家科学基金会;
关键词
stratification; bottom temperature; Cold Pool; offshore wind; Mid-Atlantic Bight; TEMPERATURE; VARIABILITY; MODEL; SALINITY; SURFACE; GULF; ROMS;
D O I
10.1093/icesjms/fsad190
中图分类号
S9 [水产、渔业];
学科分类号
0908 ;
摘要
The Mid-Atlantic Cold Pool is a seasonal mass of cold bottom water that extends throughout the Mid-Atlantic Bight (MAB). Formed from rapid vernal surface warming, the Cold Pool dissipates in the fall due to mixing events such as storms. The Cold Pool supports a myriad of MAB coastal ecosystems and economically valuable commercial and recreational fisheries. Offshore wind energy has been rapidly developing within the MAB in recent years. Studies in Europe demonstrate that offshore wind farms can impact ocean mixing and hence seasonal stratification; there is, however, limited information on how MAB wind development will affect the Cold Pool. Seasonal overlap between the Cold Pool and pre-construction wind lease areas at varying distances from shore in the MAB was evaluated using output from a data-assimilative ocean model. Results highlight overlap periods as well as a thermal gradient that persists after bottom temperatures warm above the threshold typically used to identify the Cold Pool. These results also demonstrate cross-shelf variability in Cold Pool evolution. This work highlights the need for more focused ocean modeling studies and observations of wind farm effects on the MAB coastal environment.
引用
收藏
页数:14
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