Oxygen exchange and ice melt measured at the ice-water interface by eddy correlation
[摘要] This study examined fluxes across the ice-water interface utilizing the eddycorrelation technique. Temperature eddy correlation systems were used todetermine rates of ice melting and freezing, and O2 eddy correlationsystems were used to examine O2 exchange rates driven by biological andphysical processes. The study was conducted below 0.7 m thick sea-ice inmid-March 2010 in a southwest Greenland fjord and revealed low rates of icemelt at a maximum of 0.80 mm d−1. The O2 flux associated withrelease of O2 depleted melt water was less than 13 % of the averagedaily O2 respiration rate. Ice melt and insufficient vertical turbulentmixing due to low current velocities caused periodic stratificationimmediately below the ice. This prevented the determination of fluxes 61 %of the deployment time. These time intervals were identified by examiningthe velocity and the linearity and stability of the cumulative flux. Theexamination of unstratified conditions through vertical velocity and O2spectra and their cospectra revealed characteristic fingerprints ofwell-developed turbulence. From the measured O2 fluxes aphotosynthesis/irradiance curve was established by least-squares fitting.This relation showed that light limitation of net photosynthesis began at4.2 μmol photons m−2 s−1, and that algal communities werewell-adapted to low-light conditions as they were light saturated for 75 %of the day during this early spring period. However, the sea-ice associatedmicrobial and algal community was net heterotrophic with a daily grossprimary production of 0.69 mmol O2 m−2 d−1 and a respirationrate of −2.13 mmol O2 m−2 d−1 leading to a netecosystem metabolism of −1.45 mmol O2 m−2 d−1. Thisapplication of the eddy correlation technique produced high temporalresolution O2 fluxes and ice melt rates that were measured withoutdisturbing the in situ environmental conditions while integrating over anarea of approximately 50 m2 which incorporated the highly variableactivity and spatial distributions of sea-ice communities.
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[效力级别] [学科分类] 地球化学与岩石
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