TY - JOUR
T1 - Currents and convection cause enhanced gas exchange in the ice-water boundary layer
AU - Loose, Brice
AU - Lovely, Ann
AU - Schlosser, Peter
AU - Zappa, Christopher
AU - Mcgillis, Wade
AU - Perovich, Donald
N1 - Publisher Copyright:
© 2016 B. Loose et al.
PY - 2016
Y1 - 2016
N2 - The presence of sea ice acts as a physical barrier for air-sea exchange. On the other hand it creates additional turbulence due to current shear and convection during ice formation. We present results from a laboratory study that demonstrate how shear and convection in the ice-ocean boundary layer can lead to significant gas exchange. In the absence of wind, water currents beneath the ice of 0.23m s-1 produced a gas transfer velocity (k) of 2.8m d-1, equivalent to k produced by a wind speed of 7m s-1 over the open ocean. Convection caused by air-sea heat exchange also increased k of as much as 131%compared to k produced by current shear alone. When wind and currents were combined, k increased, up to 7.6m d-1, greater than k produced by wind or currents alone, but gas exchange forcing by wind produced mixed results in these experiments. As an aggregate, these experiments indicate that using a wind speed parametrisation to estimate k in the sea ice zone may underestimate k by ca. 50 % for wind speeds < 8m s-1.
AB - The presence of sea ice acts as a physical barrier for air-sea exchange. On the other hand it creates additional turbulence due to current shear and convection during ice formation. We present results from a laboratory study that demonstrate how shear and convection in the ice-ocean boundary layer can lead to significant gas exchange. In the absence of wind, water currents beneath the ice of 0.23m s-1 produced a gas transfer velocity (k) of 2.8m d-1, equivalent to k produced by a wind speed of 7m s-1 over the open ocean. Convection caused by air-sea heat exchange also increased k of as much as 131%compared to k produced by current shear alone. When wind and currents were combined, k increased, up to 7.6m d-1, greater than k produced by wind or currents alone, but gas exchange forcing by wind produced mixed results in these experiments. As an aggregate, these experiments indicate that using a wind speed parametrisation to estimate k in the sea ice zone may underestimate k by ca. 50 % for wind speeds < 8m s-1.
KW - Air-sea gas exchange
KW - CO
KW - High latitudes
KW - Ice-ocean boundary layer
KW - Sea ice
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U2 - 10.3402/tellusb.v68.32803
DO - 10.3402/tellusb.v68.32803
M3 - Article
AN - SCOPUS:85010953471
SN - 0280-6509
VL - 68
JO - Tellus, Series B: Chemical and Physical Meteorology
JF - Tellus, Series B: Chemical and Physical Meteorology
IS - 1
M1 - 32803
ER -