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Heat and salt balances over the New England continental shelf, August 1996 to June 1997

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Field Value
Title Heat and salt balances over the New England continental shelf, August 1996 to June 1997
Names Lentz, S. J. (creator)
Shearman, R. K. (creator)
Plueddemann, A. J. (creator)
Date Issued 2010-07-29 (iso8601)
Abstract Heat and salt balances over the New England shelf are examined using 10 month time
series of currents, temperature, and salinity from a four element moored array and surface
heat and freshwater fluxes from a meteorological buoy. A principal result is closure of
the heat budget to 10 W m−2. The seasonal variation in depth‐average temperature, from
14°C in September to 5°C in March, was primarily due to the seasonal variation in surface
heat flux and a heat loss in winter caused by along‐shelf advection of colder water from the
northeast. Conductivity sensor drifts precluded closing the salt balance on time scales of
months or longer. For time scales of days to weeks, depth‐average temperature and salinity
variability were primarily due to advection. Advective heat and salt flux divergences were
strongest and most complex in winter, when there were large cross‐shelf temperature
and salinity gradients at the site due to the shelf‐slope front that separates cooler, fresher shelf
water from warmer, saltier slope water. Onshore flow of warm, salty slope water near
the bottom and offshore flow of cooler, fresher shelf water due to persistent eastward
(upwelling‐favorable) winds caused a temperature increase of nearly 3°C and a salinity
increase of 0.8 in winter. Along‐shelf barotropic tidal currents caused a temperature decrease
of 1.5°C and a salinity decrease of 0.7. Wave‐driven Stokes drift caused a temperature
increase of 0.5°C and a salinity increase of 0.4 from mid December to January when there
were large waves and large near‐surface cross‐shelf temperature and salinity gradients.
Genre Article
Topic Heat and salt balances
Identifier Lentz, S. J., R. K. Shearman, and A. J. Plueddemann (2010), Heat and salt balances over the New England continental shelf, August 1996 to June 1997, J. Geophys. Res., 115, C07017, doi:10.1029/2009JC006073.

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