Dataset Available

Dataset for: Scaling laws for the upper ocean temperature dissipation rate

Authors: Darek Bogucki
Published On: Jan 21 2016 15:07 UTC
DOI: https://doi.org/10.7266/N7KK98R4
UDI: R1.x134.073:0035
Files

Individual Files

No. of Downloads: 4

No. of Files: 4

File Size: 388.44 KB

File Format(s):
.txt

Project Information

Funded By:
Gulf of Mexico Research Initiative

Funding Cycle:
RFP-I

Research Group:
Consortium for Advanced Research on Transport of Hydrocarbon in the Environment (CARTHE)

Point of Contact

Helga S. Huntley
University of Delaware / School of Marine Science and Policy
helgah@udel.edu

Data Collection Period
2012-07-26
to
2012-07-26
Theme keywords

upper ocean, turbulence, Macando well

ISO 19115-2 Metadata
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Abstract:

Using high-resolution optical turbulence measurements, scaling laws for Chi are investigated under forcing states where either the daytime heat flux or the wind stress forcing is dominant. We find that Chi remains constant over 1.5 times the significant wave height, while over a layer below, Chi decays based on the local surface forcing. When the heat flux is dominant, traditional scaling based on the Monin-Obukhov similarity theory remains valid; Chi ∝ z^−1. When the wind stress dominates, we observe the emergence of a new scaling, Chi ∝ z^−1∕2, which is explained by invoking the effect of small-scale coherent structures on vertical heat transport. This dataset reports wind forcing, dissipation with associated depth (pressure) during the Grand Lagrangian Experiment (GLAD) July 2012. These results have implications for improved modeling of the ocean’s heat and CO2 intake. This dataset was created to support the publication Bogucki, D., et al. 2015. Scaling laws for the upper ocean temperature dissipation rate, Geophysical Research Letters doi: 10.1002/2014GL062235.

Suggested Citation:

Darek Bogucki. 2016. Dataset for: Scaling laws for the upper ocean temperature dissipation rate. Distributed by: GRIIDC, Harte Research Institute, Texas A&M University–Corpus Christi. doi:10.7266/N7KK98R4

Publications:

Bogucki, D. J., Huguenard, K., Haus, B. K., Özgökmen, T. M., Reniers, A., & Laxague, N. J. M. (2015). Scaling laws for the upper ocean temperature dissipation rate. Geophysical Research Letters, 42(3), 839–846. doi:10.1002/2014gl062235

Purpose:

To improve understanding of upper ocean fluxes

Data Parameters and Units:

File - wind.txt - column 1 = time(in second) from start time 26-Jul-2012 16:04:43 GPS; column 2 = wind speed meters per second File - pressure - column 1 = time(in second) from start time 26-Jul-2012 16:04:43 GPS; column 2 = pressure meters File - Arun_calA_chi - column 1 = time(in second) from start time 26-Jul-2012 16:04:43 GPS; column 2 = temperature dissipation Celsius^2 per second File - time_lat_lon.txt - column 1 = time(in second) from start time 26-Jul-2012 16:04:43 GPS; column 2 = latitude decimal degrees; column 3 = longitude decimal degrees

Individual Files: