Dataset: ALFA data - Indonesian Through Flow Region
View Data: Data not available yet
Data Citation:
Gomes, H. d., Goes, J. (2024) Advanced Laser Fluorescence Analyzer (ALFA) data from the Indonesian Through Flow Region from the R/V Roger Ravelle (RR2201) from January to March 2022. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2024-11-22 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/944302 [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:6.599072 E:136.543725 S:-17.186432 W:113.911019
Indonesian Through Flow Region
Temporal Extent: 2022-01-26 - 2022-03-11
Co-Principal Investigator:
Joaquim Goes (Lamont-Doherty Earth Observatory, LDEO)
Helga do Rosario Gomes (Lamont-Doherty Earth Observatory, LDEO)
Contact:
Helga do Rosario Gomes (Lamont-Doherty Earth Observatory, LDEO)
BCO-DMO Data Manager:
Karen Soenen (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version:
1
Version Date:
2024-11-22
Restricted:
No
Validated:
No
Current State:
Data not available
Advanced Laser Fluorescence Analyzer (ALFA) data from the Indonesian Through Flow Region from the R/V Roger Ravelle (RR2201) from January to March 2022
Abstract:
Underway fluoresence sampling from the western Eastern Indian Ocean Upwelling region on the R/V Roger Ravelle in January March 2022 (BLOOFINZ cruise).
Scope of the dataset is to understand the impact of the negative IOD, the anomalous warming of this region and reduced upwelling, on the community structure of phytoplankton and productivity of the Eastern Indian Ocean Upwelling Zone (EEIOUZ). As we had posited in the SCTR, that weaker upwelling in the western Equatorial Indian Ocean due to the positive phase of the IOD, would result in significant changes in the community structure of phytoplankton, their photophysiology and their nitrogenous nutrient preferences.