Abstract

Remotely sensed ocean color data are useful for monitoring water quality in coastal environments. However, moderate resolution (hundreds of meters to a few kilometers) satellite data are underutilized in these environments because of frequent data gaps from cloud cover and algorithm complexities in shallow waters. Aggregating satellite data over larger space and time scales is a common method to reduce data gaps and generate a more complete time series, but potentially smooths out the small-scale, episodic changes in water quality that can have ecological influences. By comparing aggregated satellite estimates of Kd(490) with related in-water measurements, we can understand the extent to which aggregation methods are viable for filling gaps while being able to characterize ecologically relevant water quality conditions. In this study, we tested a combination of six spatial and seven temporal scales for aggregating data from the VIIRS instrument at several coral reef locations in Maui, Hawai‘i and Puerto Rico and compared these with in situ measurements of Kd(490) and turbidity. In Maui, we found that the median value of a 5-pixels, 7-days spatiotemporal cube of satellite data yielded a robust result capable of differentiating observations across small space and time domains and had the best correlation among spatiotemporal cubes when compared with in situ Kd(490) across 11 nearshore sites (R2 = 0.84). We also found long-term averages (i.e., chronic condition) of VIIRS data using this aggregation method follow a similar spatial pattern to onshore turbidity measurements along the Maui coast over a three-year period. In Puerto Rico, we found that the median of a 13-pixels, 13-days spatiotemporal cube of satellite data yielded the best overall result with an R2 = 0.54 when compared with in situ Kd(490) measurements for one nearshore site with measurement dates spanning 2016–2019. As spatiotemporal cubes of different dimensions yielded optimum results in the two locations, we recommend local analysis of spatial and temporal optima when applying this technique elsewhere. The use of satellite data and in situ water quality measurements provide complementary information, each enhancing understanding of the issues affecting coastal ecosystems, including coral reefs, and the success of management efforts.

Highlights

  • Good water quality is essential for healthy coastal ecosystems and recent increases in land-based sources of pollution (LBSP) threaten the persistence of many ecologically important nearshore species

  • In Maui, the focus is on spatial dynamics and aggregated Visible Infrared Imaging Radiometer Suite (VIIRS) data are compared with (i) in situ nearshore optical data collected at 11 sites over three days and (ii) in situ onshore turbidity measurements collected at 51 sites over three years

  • We addressed the issue of overcoming data gaps by testing space and time aggregation methods on VIIRS data in Maui Hawai‘i and southwestern Puerto Rico to determine when the correlation with corresponding in situ measurements is optimal

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Summary

Introduction

Good water quality is essential for healthy coastal ecosystems and recent increases in land-based sources of pollution (LBSP) threaten the persistence of many ecologically important nearshore species. Human expansion has dramatically increased coastal LBSP and negatively affected water quality in nearshore environments impacting most of the world’s coral reefs (Fabricius, 2005; Sheridan et al, 2014; OtañoCruz et al, 2017). Excess sediment and nutrients that lead to eutrophication can degrade coastal ecosystem health by limiting light availability necessary for photosynthetic organisms and disrupting oligotrophic ecosystems. Coral reef ecosystems are sensitive to changes in water quality. Tropical corals live close to their upper light and temperature tolerance thresholds (Rodolfo-Metalpa et al, 2014) and, as sessile organisms, they are highly sensitive to changes in water quality, which modifies temperature, light, and availability of both beneficial and detrimental nutrients (Lesser et al, 2009). High nutrient input from terrestrial runoff can cause eutrophication that leads to phytoplankton and algae blooms, further reducing light availability

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