Revisiting Microstructure Sensor Responses with Implications for Double-Diffusive Fluxes

Revisiting Microstructure Sensor Responses with Implications for Double-Diffusive Fluxes
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DOI:
10.1175/jtech-d-12-00272.1
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发表时间:
2013-08
影响因子:
2.2
通讯作者:
T. Sommer;J. Carpenter;M. Schmid;R. Lueck;A. Wüest
T. Sommer;J. Carpenter;M. Schmid;R. Lueck;A. Wüest
中科院分区:
地球科学4区
文献类型:
--
作者:
T. Sommer;J. Carpenter;M. Schmid;R. Lueck;A. Wüest

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Thinhigh-gradientinterfacesthatoccurnaturallywithindouble-diffusivestaircasesareusedtoestimatethe response characteristics of temperature and conductivity microstructure sensors. The knowledge of these responses is essentialfor resolvingsmall-scaleturbulencein natural waterbodies and for determining doublediffusive fluxes of heat and salt. Here, the authors derive microstructure sensor responses from observed differences in the statistical distributions of interface thicknesses at various profiling speeds in Lake Kivu (central Africa). In contrast to the standard approach for determining sensor responses, this method is independent of any knowledge of the true in situ temperature and salinity structure. Assuming double-pole frequency response functions, the time constants for the Sea-Bird Electronics SBE-7 conductivity sensor and the Rockland Scientific International FP07 thermistor are estimated to be 2.2 and 10ms, respectively. In contrast to previous assumptions, the frequency response for the SBE-7 is found to be substantial and dominates the wavenumber response for profiling speeds larger than 0.19ms 21 .