| Sea wave height (m) |
WAVE |
Wave model calculating the frequency, direction and energy of waves. Spectrum that considers ocean currents and assimilates the height of significant waves based on historical altimetry records and satellite directional wave spectra. |
MFWAM model, GLORYS12, Sentinel 1 SAR. Temporal resolution three hourly instantaneous at 20 km2 from 2007 to 2016. |
None*
|
| Sea surface temperature (°C) |
SST |
Monthly nighttime temperatures of the sea surface, data derived from satellites infrared observations. |
MODIS Global Mapped 11 µm Nighttime Sea Surface Temperature (NSST) from Terra and Aqua satellites, monthly at 4 km from 2007 to 2016. |
Kilpatrick et al. (2015)
**
|
| Degree heating week (°C) |
DHW |
Sum of the weekly positive anomaly of the nocturnal sea surface temperature, compared to the monthly maximum of the adjusted climatology, over a 12 week period. |
SATcoral-SIMAR product according to NOAA Coral Reef Watch methodologies using weekly data from OSTIA and GHRSST-MUR, at 1 km from 2007 to 2016. |
Cerdeira-Estrada et al. (2019)
***
|
| Chlorophyll-a concentration (mg m−3) |
CHL1 |
Chlorophyll-a concentration according to the GSM method, from the reflectance normalized to the original wavelengths of the sensor, without intercalibration. Variable widely used to estimate phytoplankton concentrations. |
MODIS sensor on the AQUA satellite. Monthly data at 4 km from 2007 to 2016. |
O’Reilly et al (2000)
**
|
| Particulate organic carbon (mol m−3) |
POC |
Important component of the carbon cycle obtained from the original NASA algorithm (correlation of band proportions). It is considered a proxy for particulate organic matter. |
MODIS sensor on the AQUA satellite. Monthly data at 4 km from 2007 to 2016. |
Stramski et al. (2008)
**
|
| Photosynthetically available radiation (Einstein m−2 day−1) |
PAR |
Daily average of the photon flux density within the visible range (400–700 nm) of the light spectrum. Usable light in photosynthetic processes. |
MODIS sensor on the AQUA satellite. Monthly data at 4 km from 2007 to 2016. |
Frouin, Franz & Werdell (2003)
**
|
| Diffuse attenuation coefficient (m−1) |
KD490 |
Based on the downwelling irradiance attenuation at 490 nm. Is obtained from the Morel algorithm. Considered a proxy of seawater turbidity. |
MODIS sensor on the AQUA satellite. Monthly data at 4 km from 2007 to 2016. |
Morel et al. (2007)
**
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