2018
DOI: 10.13053/rcs-147-12-20
|View full text |Cite
|
Sign up to set email alerts
|

Spatio-Temporal Assessment of "Chlorophyll a" in Banco Chinchorro using Remote Sensing

Abstract: Quantitative assessments of the temporal variances of physical and biological phenomena are very useful for the understanding of ecosystem functioning. Marine ecosystems are very complex, and regarding biodiversity and fishing resources, Banco Chinchorro (BCh) is one of the most important in the south of the Yucatan Peninsula. Additionally, BCh is an important hotspot of assimilation and release of carbon, for which hurricanes play a supporting role by mixing deep and superficial water masses affecting nutrien… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2019
2019
2022
2022

Publication Types

Select...
2
1

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(1 citation statement)
references
References 9 publications
0
1
0
Order By: Relevance
“…Another link between TC physical attributes (e.g., strength, trajectory) and ecosystem function is the spatiotemporal variation of Chl-a along the YP coastal zone. Our comparative analysis shows a significant increase in Chl-a after TC passage along with localized impacts depending on the storm exit point along the coast; this increase has been observed in other regions of the CS, west of the YP (e.g., Banco Chinchorro, Figure 1B; [117]). By considering a concentration of 0.5 mg/m 3 as an average baseline, we identified enhanced areas (>15,000 km 2 , Figure 10B) with concentrations >0.5 mg/m 3 after the passage of Stan and Emily.…”
Section: Tc Impacts On Terrestrial Vegetation and Chl-a Concentration In Coastal Watersmentioning
confidence: 52%
“…Another link between TC physical attributes (e.g., strength, trajectory) and ecosystem function is the spatiotemporal variation of Chl-a along the YP coastal zone. Our comparative analysis shows a significant increase in Chl-a after TC passage along with localized impacts depending on the storm exit point along the coast; this increase has been observed in other regions of the CS, west of the YP (e.g., Banco Chinchorro, Figure 1B; [117]). By considering a concentration of 0.5 mg/m 3 as an average baseline, we identified enhanced areas (>15,000 km 2 , Figure 10B) with concentrations >0.5 mg/m 3 after the passage of Stan and Emily.…”
Section: Tc Impacts On Terrestrial Vegetation and Chl-a Concentration In Coastal Watersmentioning
confidence: 52%