scholarly journals Tidally-driven interannual variation in extreme sea level probabilities in the Gulf of Maine

2020 ◽  
Author(s):  
Hannah Baranes ◽  
Jonathan Woodruff ◽  
Stefan Talke ◽  
Robert Kopp ◽  
Richard Ray ◽  
...  
2020 ◽  
Vol 125 (10) ◽  
Author(s):  
H. E. Baranes ◽  
J. D. Woodruff ◽  
S. A. Talke ◽  
R. E. Kopp ◽  
R. D. Ray ◽  
...  

2020 ◽  
Author(s):  
Hannah Baranes ◽  
Jonathan Woodruff ◽  
Stefan Talke ◽  
Robert Kopp ◽  
Richard Ray ◽  
...  

Energy ◽  
2019 ◽  
Vol 187 ◽  
pp. 115942 ◽  
Author(s):  
Boma Kresning ◽  
M. Reza Hashemi ◽  
Simon P. Neill ◽  
J. A. Mattias Green ◽  
Huijie Xue

2018 ◽  
Vol 99 (6) ◽  
pp. 1155-1176 ◽  
Author(s):  
Robert M. Banta ◽  
Yelena L. Pichugina ◽  
W. Alan Brewer ◽  
Eric P. James ◽  
Joseph B. Olson ◽  
...  

AbstractTo advance the understanding of meteorological processes in offshore coastal regions, the spatial variability of wind profiles must be characterized and uncertainties (errors) in NWP model wind forecasts quantified. These gaps are especially critical for the new offshore wind energy industry, where wind profile measurements in the marine atmospheric layer spanned by wind turbine rotor blades, generally 50–200 m above mean sea level (MSL), have been largely unavailable. Here, high-quality wind profile measurements were available every 15 min from the National Oceanic and Atmospheric Administration/Earth System Research Laboratory (NOAA/ESRL)’s high-resolution Doppler lidar (HRDL) during a monthlong research cruise in the Gulf of Maine for the 2004 New England Air Quality Study. These measurements were compared with retrospective NWP model wind forecasts over the area using two NOAA forecast-modeling systems [North American Mesoscale Forecast System (NAM) and Rapid Refresh (RAP)]. HRDL profile measurements quantified model errors, including their dependence on height above sea level, diurnal cycle, and forecast lead time. Typical model wind speed errors were ∼2.5 m s−1, and vector-wind errors were ∼4 m s−1. Short-term forecast errors were larger near the surface—30% larger below 100 m than above and largest for several hours after local midnight (biased low). Longer-term, 12-h forecasts had the largest errors after local sunset (biased high). At more than 3-h lead times, predictions from finer-resolution models exhibited larger errors. Horizontal variability of winds, measured as the ship traversed the Gulf of Maine, was significant and raised questions about whether modeled fields, which appeared smooth in comparison, were capturing this variability. If not, horizontal arrays of high-quality, vertical-profiling devices will be required for wind energy resource assessment offshore. Such measurement arrays are also needed to improve NWP models.


The Holocene ◽  
2002 ◽  
Vol 12 (4) ◽  
pp. 383-389 ◽  
Author(s):  
W. Roland Gehrels ◽  
Daniel F. Belknap ◽  
Stuart Black ◽  
Rewi M. Newnham

1985 ◽  
Vol 24 (2) ◽  
pp. 187-196 ◽  
Author(s):  
R.N. Oldale

Seismic profiles across the southwest end of Jeffreys Ledge, a bathymetric high north of Cape Ann, Massachusetts, reveal two end moraines. The moraines overlie upper Wisconsinan glacialmarine silty clay and are composed mostly of subaqueous ice-contact deposits and outwash. They were formed below sea level in water depths of as much as 120 m during fluctuations of a calving ice front. The moraines are late Wisconsinan in age and were formed after the Cambridge readvance, about 14,000 yr B.P., and before the Kennebunk readvance, about 13,000 yr B.P. They represent fluctuations of the ice front during overall retreat of Laurentide ice from the Gulf of Maine and New England.


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