©2020 Biological and Chemical Oceanography Data Management Office.Funded by the U.S. National Science Foundation
Heat has been widely used as an inexpensive tracer in groundwater systems (Anderson 2005; Constanz 2008), including studies of SGD (Taniguchi 2000; Moore and Wilson 2005; Martin et al 2006). In our system, the temperature of sub-seafloor porewaters differs from the temperature of overlying seawater owing to seasonal variations in surface temperature. We can thus use heat in two ways: (1) to measure the depth of rapid flushing events and (2) to estimate rates of long-term regional flow.
Heat has been widely used as an inexpensive tracer in groundwater systems (Anderson 2005; Constanz 2008), including studies of SGD (Taniguchi 2000; Moore and Wilson 2005; Martin et al 2006). In our system, the temperature of sub-seafloor porewaters differs from the temperature of overlying seawater owing to seasonal variations in surface temperature. We can thus use heat in two ways: (1) to measure the depth of rapid flushing events and (2) to estimate rates of long-term regional flow.
Wilson, A. M., White, S. M., Moore, W. S. (2019) Temperature profiles collected from the sediments off the South Atlantic Bight from 2015-05-01 to 2017-05-10. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 0) Version Date 2019-12-30 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/785219 [access date]
Terms of Use
This dataset is licensed under Creative Commons Attribution 4.0.
If you wish to use this dataset, it is highly recommended that you contact the original principal investigators (PI). Should the relevant PI be unavailable, please contact BCO-DMO (info@bco-dmo.org) for additional guidance. For general guidance please see the BCO-DMO Terms of Use document.
©2020 Biological and Chemical Oceanography Data Management Office.