Bleaching and environmental data for global coral reef sites from 1980-2020

Website: https://www.bco-dmo.org/dataset/773466
Data Type: Other Field Results
Version: 2
Version Date: 2022-10-14

Project
» Identifying coral reef 'bright spots' from the global 2015-2017 thermal-stress event (Coral Reef Brightspots)
ContributorsAffiliationRole
van Woesik, RobertFlorida Institute of Technology (FIT)Principal Investigator, Contact
Burkepile, DeronUniversity of California-Santa Barbara (UCSB)Co-Principal Investigator
Kratochwill, ChelseyFlorida Institute of Technology (FIT)Data Manager
Rauch, ShannonWoods Hole Oceanographic Institution (WHOI BCO-DMO)BCO-DMO Data Manager

Abstract
These data include information on the presence and absence of coral bleaching, allowing comparative analyses and the determination of geographical bleaching thresholds, together with site exposure, distance to land, mean turbidity, cyclone frequency, and a suite of sea-surface temperature metrics at the times of survey.


Coverage

Spatial Extent: N:36.75 E:179.964472 S:-30.2625 W:-179.974333
Temporal Extent: 1980-06-15 - 2020-08-15

Methods & Sampling

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 Description

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.


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Data Files

File
global_bleaching_environmental.csv
(Comma Separated Values (.csv), 16.00 MB)
MD5:42a6f10a6efa9e6b926d04b86b45a19f
Primary data file for dataset ID 773466

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Related Publications

Donner, S. D., Rickbeil, G. J. M., & Heron, S. F. (2017). A new, high-resolution global mass coral bleaching database. PLOS ONE, 12(4), e0175490. https://doi.org/10.1371/journal.pone.0175490
Methods
Donovan, M. K., Burkepile, D. E., Kratochwill, C., Shlesinger, T., Sully, S., Oliver, T. A., Hodgson, G., Freiwald, J., & van Woesik, R. (2021). Local conditions magnify coral loss after marine heatwaves. Science, 372(6545), 977–980. https://doi.org/10.1126/science.abd9464
Results
Florida Reef Resilience Program’s Disturbance Response Monitoring 2005–2020. Unpublished data. Florida Fish and Wildlife Conservation Commission. Environmental Protection Agency cooperative agreement number X7-01D00320-0. https://ocean.floridamarine.org/FRRP/ (2020).
Methods
Hodgson, G. (1999). A Global Assessment of Human Effects on Coral Reefs. Marine Pollution Bulletin, 38(5), 345–355. https://doi.org/10.1016/s0025-326x(99)00002-8 https://doi.org/10.1016/S0025-326X(99)00002-8
Methods
Kumagai, N. H., & Yamano, H. (2018). High-resolution modeling of thermal thresholds and environmental influences on coral bleaching for local and regional reef management. PeerJ, 6, e4382. Portico. https://doi.org/10.7717/peerj.4382
Methods
Marks, K.W. AGRRA Database, version (2018-03). http:www.agrra.org/data-explorer/explore-summary-products/ (2018).
Methods
McClanahan, T. R., Darling, E. S., Maina, J. M., Muthiga, N. A., ’agata, S. D., Jupiter, S. D., Arthur, R., Wilson, S. K., Mangubhai, S., Nand, Y., Ussi, A. M., Humphries, A. T., Patankar, V. J., Guillaume, M. M. M., Keith, S. A., Shedrawi, G., Julius, P., Grimsditch, G., Ndagala, J., & Leblond, J. (2019). Temperature patterns and mechanisms influencing coral bleaching during the 2016 El Niño. Nature Climate Change, 9(11), 845–851. https://doi.org/10.1038/s41558-019-0576-8
Methods
Safaie, A., Silbiger, N. J., McClanahan, T. R., Pawlak, G., Barshis, D. J., Hench, J. L., Rogers, J. S., Williams, G. J., & Davis, K. A. (2018). High frequency temperature variability reduces the risk of coral bleaching. Nature Communications, 9(1). https://doi.org/10.1038/s41467-018-04074-2
Methods
Saha, K., Zhao, X., Zhang, H.-M., Casey, K. S., Zhang, D., Zhang, Y., Baker-Yeboah, S., Relph, J. M., Krishnan, A., & Ryan, T. (2018). The Coral Reef Temperature Anomaly Database (CoRTAD) Version 6 - Global, 4 km Sea Surface Temperature and Related Thermal Stress Metrics for 1982 to 2019 [Data set]. NOAA National Centers for Environmental Information. https://doi.org/10.25921/FFW7-CS39 https://doi.org/10.25921/ffw7-cs39
Methods
Spalding, M. D., Fox, H. E., Allen, G. R., Davidson, N., Ferdaña, Z. A., Finlayson, M., Halpern, B. S., Jorge, M. A., Lombana, A., Lourie, S. A., Martin, K. D., McManus, E., Molnar, J., Recchia, C. A., & Robertson, J. (2007). Marine Ecoregions of the World: A Bioregionalization of Coastal and Shelf Areas. BioScience, 57(7), 573–583. https://doi.org/10.1641/b570707 https://doi.org/10.1641/B570707
Methods
Sully, S., & Woesik, R. (2020). Turbid reefs moderate coral bleaching under climate‐related temperature stress. Global Change Biology, 26(3), 1367–1373. Portico. https://doi.org/10.1111/gcb.14948
Results
Sully, S., Burkepile, D. E., Donovan, M. K., Hodgson, G., & van Woesik, R. (2019). A global analysis of coral bleaching over the past two decades. Nature Communications, 10(1). doi:10.1038/s41467-019-09238-2
Results
Veron, J., Stafford-Smith, M., DeVantier, L., & Turak, E. (2015). Overview of distribution patterns of zooxanthellate Scleractinia. Frontiers in Marine Science, 1. doi:10.3389/fmars.2014.00081
Methods
van Woesik, R., & Kratochwill, C. (2022). A global coral-bleaching database, 1980–2020. Scientific Data, 9(1). https://doi.org/10.1038/s41597-022-01121-y
Results

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Related Datasets

Different Version
van Woesik, R., & Kratochwill, C. (2022). A Global Coral-Bleaching Database (GCBD), 1998–2020. figshare. https://doi.org/10.6084/M9.FIGSHARE.C.5314466 https://doi.org/10.6084/m9.figshare.c.5314466

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Parameters

ParameterDescriptionUnits
Site_IDUnique identifier for each site unitless
Sample_IDUnique identifier for each sampling event unitless
Data_SourceSource of data set unitless
Latitude_DegreesLatitude coordinates (positive vaues = North; negative values = South) degrees North
Longitude_DegreesLongitude coordinates (positive values = East; negative values = West) degrees East
Ocean_NameThe ocean in which the sampling took place unitless
Reef_IDUnique identifier from Reef Check data unitless
Realm_NameIdentification of realm as defined by the Marine Ecoregions of the World (MEOW) Spalding et al. 2007 unitless
Ecoregion_NameIdentification of the Ecoregions (150) as defined by Veron et al unitless
Country_NameThe country where sampling took place unitless
State_Island_Province_NameThe state, territory (e.g., Guam) or island group (e.g., Hawaiian Islands) where sampling took place unitless
City_Town_NameThe region, city, or nearest town, where sampling took place unitless
Site_NameThe accepted name of the site or the name given by the team that sampled the reef unitless
Distance_to_ShoreThe distance of the sampling site from the nearest land meters (m)
ExposureThe 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
TurbidityKd490 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_Frequencynumber of cyclone events from 1964 to 2014 unitless
Date_Daythe day of the sampling event unitless
Date_Monththe month of sampling event unitless
Date_Yearthe year of sampling event unitless
Depth_mdepth of sampling site meters (m)
Substrate_Nametype of substrate from Reef Check data unitless
Percent_Coveraverage cover value (percent) percent
Bleaching_LevelReef Check data, coral population or coral colony unitless
Percent_BleachingAn average of four transect segments (Reef Check) or average of a bleaching code percent
ClimSSTClimatological sea surface temperature (SST) based on weekly SSTs for the study time frame, created using a harmonics approach degrees Celsius
Temperature_KelvinTemperature in Kelvin Kelvin
Temperature_MeanMean Temperature degrees Celsius
Temperature_MinimumMinimum Temperture degrees Celsius
Temperature_MaximumMaximum Temperature degrees Celsius
Temperature_Kelvin_Standard_DeviationStandard deviation of temperature Kelvin
WindspeedWindspeed meters per hour
SSTASea Surface Temperature Anomaly: weekly SST minus weekly climatological SST degrees Celsius
SSTA_Standard_DeviationThe Standard Deviation of weekly SST Anomalies over the entire time period degrees Celsius
SSTA_MeanThe mean SSTA over the entire time period degrees Celsius
SSTA_MinimumThe minimum SSTA over the entire time period degrees Celsius
SSTA_MaximumThe maximum SSTA over the entire time period degrees Celsius
SSTA_FrequencySea Surface Temperature Anomaly Frequency: number of times over the previous 52 weeks that SSTA >=1 degree C SSTA per time period
SSTA_Frequency_Standard_DeviationThe standard deviation of SSTA_Frequency over the entire time period SSTA per time period
SSTA_FrequencyMaxThe maximum SSTA_Frequency over the entire time period SSTA per time period
SSTA_FrequencyMeanThe mean SSTA_Frequency over the entire time period SSTA per time period
SSTA_DHWSea Surface Temperature Degree Heating Weeks: sum of previous 12 weeks when SSTA>=1 degree C weeks
SSTA_DHW_Standard_DeviationThe standard deviation SSTA_DHW over the entire time period weeks
SSTA_DHWMaxThe maximum SSTA_DHW over the entire time period weeks
SSTA_DHWMeanThe mean SSTA_DHW over the entire time period weeks
TSAThermal Stress Anomaly: Weekly sea surface temperature minus the maximum of weekly climatological sea surface temperature degrees Celsius
TSA_Standard_DeviationThe standard deviation of TSA over the entire time period degrees Celsius
TSA_MinimumThe minimum TSA over the entire time period degrees Celsius
TSA_MaximumThe maximum TSA over the entire time period degrees Celsius
TSA_MeanThe mean TSA over the entire times period degrees Celsius
TSA_FrequencyThermal Stress Anomaly Frequency: number of times over previous 52 weeks that TSA >=1 degree C TSA per time period
TSA_Frequency_Standard_DeviationThe standard deviation of frequency of thermal stress anomalies over the entire time period TSA per time period
TSA_FrequencyMaxThe maximum TSA_Frequency over the entire time period TSA per time period
TSA_FrequencyMeanThe mean TSA_Frequency over the entire time period TSA per time period
TSA_DHWThermal Stress Anomaly (TSA) Degree Heating Week (DHW): Sum of previous 12 weeks when TSA >=1 degree C weeks
TSA_DHW_Standard_DeviationThe standard deviation of TSA_DHW over the entire time period weeks
TSA_DHWMaxThe maximum TSA_DHW over the entire time period weeks
TSA_DHWMeanThe mean TSA_DHW over the entire time period weeks
Datedate of sampling event in format YYYY-MM-DD unitless
Site_Commentscomments of any issues with the site or additional information unitless
Sample_Commentscomments of any issue or additional information of sampling event unitless
Bleaching_Commentscomments of any issue or additional information of bleaching value unitless

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Project Information

Identifying coral reef 'bright spots' from the global 2015-2017 thermal-stress event (Coral Reef Brightspots)

Coverage: Global


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.



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Funding

Funding SourceAward
NSF Division of Ocean Sciences (NSF OCE)

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