Dataset: Galveston Bay Pigments
View Data: Data not available yet
Data Citation:
Liu, H., Hu, X., Dias, L. M. (2024) Galveston Bay Pigments. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-11-19 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/943964 [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.
Spatial Extent: N:30 E:95.5 S:29 W:94.5
Galveston Bay, an estuary situated adjacent to the Northwestern Gulf of Mexico
Temporal Extent: 2017-10-22 - 2018-10-14
Project:
RAPID: Capturing the Signature of Hurricane Harvey on Texas Coastal Lagoons
(Hurricane Harvey Texas Lagoons)
Principal Investigator:
Hui Liu (Texas A&M, Galveston, TAMUG)
Co-Principal Investigator:
Xinping Hu (Texas A&M, Corpus Christi, TAMU-CC)
Scientist:
Larissa Marie Dias (Texas A&M, Corpus Christi, TAMU-CC)
Contact:
Larissa Marie Dias (Texas A&M, Corpus Christi, TAMU-CC)
BCO-DMO Data Manager:
Sawyer Newman (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2024-11-19
Restricted:
No
Validated:
No
Current State:
Preliminary and in progress
Abstract:
Quantifying the direction and magnitude of CO2 flux in estuaries is necessary to constrain the global carbon cycle, yet carbonate systems and CO2 flux in subtropical and urbanized estuaries are not yet fully determined. To estimate the CO2 flux for Galveston Bay, a subtropical estuary located in the northwestern Gulf of Mexico proximal to the Houston-Galveston metroplex, monthly cruises were conducted along a transect extending from the Houston ship channel to the mouth of Galveston Bay and Gulf of Mexico from October 2017 to September 2018. Surface samples were collected at each of five stations in the Bay and analyzed for chlorophyll-a. Chlorophyll-a concentrations varied spatially and temporally throughout the study period and were highest in the inner Bay in late winter (February) and at all stations in mid-spring (April), following the freshwater inflow event. Stations 4 and 5 (inner Bay, closest to the San Jacinto River mouth) had early peak chlorophyll-a concentrations in February of 2018 (39.9 and 63.3 µg L-1, respectively), whereas mid- and outermost sampling locations 1, 2, and 3 peaked in mid-April (28.2, 44.2, and 35.8 µg L-1, respectively). Slight increases in chlorophyll-a were observed at stations 4 and 5 in July and September of 2018. When compared with carbonate chemistry data, it appears that large freshwater inflows in late winter and early spring stimulated photosynthesis in the Bay, leading to an influx of atmospheric CO2.