Contributors | Affiliation | Role |
---|---|---|
van Woesik, Robert | Florida Institute of Technology (FIT) | Principal Investigator, Contact |
Burkepile, Deron | University of California-Santa Barbara (UCSB) | Co-Principal Investigator |
Kratochwill, Chelsey | Florida Institute of Technology (FIT) | Data Manager |
Rauch, Shannon | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
See Methods of van Woesik and Kratochwill (2022; doi: 10.1038/s41597-022-01121-y)
Briefly, data were collected from seven sources: 1) Reef Check (https://www.reefcheck.org/global-reef-tracker/), (2) Donner et al. (2017), (3) McClanahan et al. (2019), (4) AGRRA (https://www.agrra.org), (5) FRRP (https://ocean.floridamarine.org/FRRP/Home/Reports), (6) Safaie et al. (2018), and (7) Kumagai et al. (2018). Site coordinates were standardized to decimal degrees using Google Earth. Coordinates were compared to ensure a sampling event was not duplicated across multiple data sources. Points were removed if they occurred on land or were more than 1 kilometer from a coral reef. Environmental and site data were added to each site, including reef site exposure, distance to land, mean turbidity, cyclone frequency, and CoRTAD Version 6 environmental data.
Data processing:
Data were processed using Microsoft Access 2019, R, and QGIS.
Known problems/issues:
There were few data on coral bleaching before the 1998 bleaching event and most data were collected between 2015 and 2016.
BCO-DMO Processing:
version 1:
(date: 2019-07-18)
- renamed "Latitude Degrees" to "Latitude_Degrees";
- replaced blanks (no data) with "nd";
- removed special characters from place names;
- added "Date2" column with date formatted as yyyymmdd.
version 2:
(date: 2022-10-14)
- created "Date" field from separate year, month, day columns;
- removed commas from: "Ecoregion", "City_Town_Name", "Site_Name";
- replaced commas with semi-colons in: "Sample_Comments", "Site_Comments";
- replaced or removed line breaks (\n, \r, <br>) and tabs (\t) with spaces in: "Sample_Comments", "Site_Comments";
- replaced or removed non-printing characters;
- reordered fields (moved comments to the end for readability);
- rounded latitude, longitude, and turbidity columns to 4 decimal places;
- rounded all other numeric columns to 2 decimal places.
File |
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global_bleaching_environmental.csv (Comma Separated Values (.csv), 16.00 MB) MD5:42a6f10a6efa9e6b926d04b86b45a19f Primary data file for dataset ID 773466 |
Parameter | Description | Units |
Site_ID | Unique identifier for each site | unitless |
Sample_ID | Unique identifier for each sampling event | unitless |
Data_Source | Source of data set | unitless |
Latitude_Degrees | Latitude coordinates (positive vaues = North; negative values = South) | degrees North |
Longitude_Degrees | Longitude coordinates (positive values = East; negative values = West) | degrees East |
Ocean_Name | The ocean in which the sampling took place | unitless |
Reef_ID | Unique identifier from Reef Check data | unitless |
Realm_Name | Identification of realm as defined by the Marine Ecoregions of the World (MEOW) Spalding et al. 2007 | unitless |
Ecoregion_Name | Identification of the Ecoregions (150) as defined by Veron et al | unitless |
Country_Name | The country where sampling took place | unitless |
State_Island_Province_Name | The state, territory (e.g., Guam) or island group (e.g., Hawaiian Islands) where sampling took place | unitless |
City_Town_Name | The region, city, or nearest town, where sampling took place | unitless |
Site_Name | The accepted name of the site or the name given by the team that sampled the reef | unitless |
Distance_to_Shore | The distance of the sampling site from the nearest land | meters (m) |
Exposure | The site's exposure to fetch. Site was considered exposed if it had >20 km of fetch, if there were strong seasonal winds, or if the site faced the prevailing winds. Otherwise, the site was considered sheltered or "sometimes". "Sometimes" refers to a few sites with a >20 km fetch through a narrow geographic window, and therefore we considered that the site was potentially exposed during cyclone seasons. | unitless |
Turbidity | Kd490 with a 100-km buffer. Turbidity was considered to be positively related to the diffuse attenuation coefficient of light at the 490 nm wavelength (Kd490), or the rate at which light at 490 nm is attenuated with depth. For example, a Kd490 value of 0.1 m?1 means that light intensity is reduced by one natural-log value within 10 m of water. High values of Kd490, therefore, represent high attenuation and hence high turbidity. | reciprocal meters (m-1) |
Cyclone_Frequency | number of cyclone events from 1964 to 2014 | unitless |
Date_Day | the day of the sampling event | unitless |
Date_Month | the month of sampling event | unitless |
Date_Year | the year of sampling event | unitless |
Depth_m | depth of sampling site | meters (m) |
Substrate_Name | type of substrate from Reef Check data | unitless |
Percent_Cover | average cover value (percent) | percent |
Bleaching_Level | Reef Check data, coral population or coral colony | unitless |
Percent_Bleaching | An average of four transect segments (Reef Check) or average of a bleaching code | percent |
ClimSST | Climatological sea surface temperature (SST) based on weekly SSTs for the study time frame, created using a harmonics approach | degrees Celsius |
Temperature_Kelvin | Temperature in Kelvin | Kelvin |
Temperature_Mean | Mean Temperature | degrees Celsius |
Temperature_Minimum | Minimum Temperture | degrees Celsius |
Temperature_Maximum | Maximum Temperature | degrees Celsius |
Temperature_Kelvin_Standard_Deviation | Standard deviation of temperature | Kelvin |
Windspeed | Windspeed | meters per hour |
SSTA | Sea Surface Temperature Anomaly: weekly SST minus weekly climatological SST | degrees Celsius |
SSTA_Standard_Deviation | The Standard Deviation of weekly SST Anomalies over the entire time period | degrees Celsius |
SSTA_Mean | The mean SSTA over the entire time period | degrees Celsius |
SSTA_Minimum | The minimum SSTA over the entire time period | degrees Celsius |
SSTA_Maximum | The maximum SSTA over the entire time period | degrees Celsius |
SSTA_Frequency | Sea Surface Temperature Anomaly Frequency: number of times over the previous 52 weeks that SSTA >=1 degree C | SSTA per time period |
SSTA_Frequency_Standard_Deviation | The standard deviation of SSTA_Frequency over the entire time period | SSTA per time period |
SSTA_FrequencyMax | The maximum SSTA_Frequency over the entire time period | SSTA per time period |
SSTA_FrequencyMean | The mean SSTA_Frequency over the entire time period | SSTA per time period |
SSTA_DHW | Sea Surface Temperature Degree Heating Weeks: sum of previous 12 weeks when SSTA>=1 degree C | weeks |
SSTA_DHW_Standard_Deviation | The standard deviation SSTA_DHW over the entire time period | weeks |
SSTA_DHWMax | The maximum SSTA_DHW over the entire time period | weeks |
SSTA_DHWMean | The mean SSTA_DHW over the entire time period | weeks |
TSA | Thermal Stress Anomaly: Weekly sea surface temperature minus the maximum of weekly climatological sea surface temperature | degrees Celsius |
TSA_Standard_Deviation | The standard deviation of TSA over the entire time period | degrees Celsius |
TSA_Minimum | The minimum TSA over the entire time period | degrees Celsius |
TSA_Maximum | The maximum TSA over the entire time period | degrees Celsius |
TSA_Mean | The mean TSA over the entire times period | degrees Celsius |
TSA_Frequency | Thermal Stress Anomaly Frequency: number of times over previous 52 weeks that TSA >=1 degree C | TSA per time period |
TSA_Frequency_Standard_Deviation | The standard deviation of frequency of thermal stress anomalies over the entire time period | TSA per time period |
TSA_FrequencyMax | The maximum TSA_Frequency over the entire time period | TSA per time period |
TSA_FrequencyMean | The mean TSA_Frequency over the entire time period | TSA per time period |
TSA_DHW | Thermal Stress Anomaly (TSA) Degree Heating Week (DHW): Sum of previous 12 weeks when TSA >=1 degree C | weeks |
TSA_DHW_Standard_Deviation | The standard deviation of TSA_DHW over the entire time period | weeks |
TSA_DHWMax | The maximum TSA_DHW over the entire time period | weeks |
TSA_DHWMean | The mean TSA_DHW over the entire time period | weeks |
Date | date of sampling event in format YYYY-MM-DD | unitless |
Site_Comments | comments of any issues with the site or additional information | unitless |
Sample_Comments | comments of any issue or additional information of sampling event | unitless |
Bleaching_Comments | comments of any issue or additional information of bleaching value | unitless |
NSF Award Abstract:
Coral reefs are one of the world's most diverse ecosystems that provide goods and services, such as fisheries and storm protection, for inhabitants of tropical and subtropical regions. However, the current rapid rate of climate change threatens the existence of coral reefs as they degrade because of thermal-stress events. Consequently, the coverage and coral composition of many coral reefs is changing. Most global models suggest that few if any reef corals will survive beyond the 2.5 degree Celsius temperature rise predicted for the tropical oceans within the next hundred years. Such predictions differ from recent field studies on coral reefs that show pockets where corals do not bleach and die. The disagreement between the global models and field assessments is a consequence of ignoring climate-change refuges; it is critical to locate the climate-change refuges and determine what circumstances are conducive for coral survival. The investigators will examine the global response of coral reefs to thermal stresses over the last two decades, and focus on the 2015-2017 El Nino event, which caused considerable thermal stress and coral bleaching. The investigators ask the question: Where are the coral reef 'bright spots' from the thermal-stress events? 'Bright spots' are considered as places with less than expected bleaching. The team will also assess why some localities are potential 'bright spots'. Identifying coral reef bright spots will help guide future conservation decisions by enabling managers to target reefs with specific characteristics, which could be protected from human encroachment and be designated as potential refuges from coral bleaching as climate change progresses. This project includes training of a post-doctoral fellow and a Ph.D student, and host a coral-bleaching workshop. This study will be of relevance to all persons that live and work near coral reefs. What happens to reef corals has cascading consequences on other reef-associated organisms, and also influences whether reefs can keep up with sea-level rise.
The current rapid rate of climate change threatens the existence of coral reefs as they degrade by thermal-stress events. A glimmer of optimism lies in the observation that thermal stresses vary spatially and temporally across the oceans, with the consequence that coral communities in different geographic regions, and under different local conditions, are likely to inherently differ in their capacity to tolerate thermal stress. One of the most transformative aspects of this work is in analyzing the extent to which the bleaching patterns differed from model predictions. This work will capitalize on the recent progress on Bright-Spots Analysis to assess unexpected outcomes. The investigators will take two approaches. First, the project will use a machine-learning algorithm, boosted regression trees to examine the relationships between coral bleaching and the environmental predictor variables of interest. Second, a series of generalized mixed effects models, within a hierarchical Bayesian framework, will be used to identify where geographically 'bright spots' from thermal stress are located and why some coral reefs are more susceptible to thermal stresses than others.
Funding Source | Award |
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NSF Division of Ocean Sciences (NSF OCE) |