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CRED Coral Reef Early Warning System (CREWS) Standard Buoy, Supplemental Sea Surface Temperature Recorder (SBE39); NWHI, MAR; Long: -170.63378, Lat: 25.44642 (WGS84); Sensor Depth: 1.00m; Data Range: 20060915-20080918.

Data provided by  National Oceanic and Atmospheric Administration

CREWS Standard (CREWS-STD) buoys are equipped to measure sea surface water temperature and conductivity (Sea-Bird Model SBE37-SM, Sea-Bird Electronics, Inc., www.seabird.com) at 1 m (nominal) below the water line and air temperature (R.M Young Model 41342); barometric pressure (Heise DXD and wind vectors (Vaisala WAS425A) at 2 m (nominal) above the water line. A compass (KVH C100 SE-25) is used in the calculation of wind direction and a GPS system provides geolocation.

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Modified: 2025-04-21

CRED Coral Reef Early Warning System (CREWS) Standard Buoy, Sea Surface Temperature and Conductivity Recorder (SBE37); NWHI, PHR; Long: -175.81612, Lat: 27.85325 (WGS84); Sensor Depth: 1.00m; Data Range: 20020918-20030314.

Data provided by  National Oceanic and Atmospheric Administration

CREWS Standard (CREWS-STD) buoys are equipped to measure sea surface water temperature and conductivity (Sea-Bird Model SBE37-SM, Sea-Bird Electronics, Inc., www.seabird.com) at 1 m (nominal) below the water line and air temperature (R.M Young Model 41342); barometric pressure (Heise DXD and wind vectors (Vaisala WAS425A) at 2 m (nominal) above the water line. A compass (KVH C100 SE-25) is used in the calculation of wind direction and a GPS system provides geolocation.

Tags:

Modified: 2025-04-21

CRED Coral Reef Early Warning System (CREWS) Standard Buoy, Sea Surface Temperature and Conductivity Recorder (SBE37); NWHI, PHR; Long: -175.81593, Lat: 27.85397 (WGS84); Sensor Depth: 1.00m; Data Range: 20040927-20060912.

Data provided by  National Oceanic and Atmospheric Administration

CREWS Standard (CREWS-STD) buoys are equipped to measure sea surface water temperature and conductivity (Sea-Bird Model SBE37-SM, Sea-Bird Electronics, Inc., www.seabird.com) at 1 m (nominal) below the water line and air temperature (R.M Young Model 41342); barometric pressure (Heise DXD and wind vectors (Vaisala WAS425A) at 2 m (nominal) above the water line. A compass (KVH C100 SE-25) is used in the calculation of wind direction and a GPS system provides geolocation.

Tags:

Modified: 2025-04-21

CRED Coral Reef Early Warning System (CREWS) Standard Buoy, Supplemental Sea Surface Temperature Recorder (SBE39); NWHI, PHR; Long: -175.81590, Lat: 27.85408 (WGS84); Sensor Depth: 0.50m; Data Range: 20030801-20030810.

Data provided by  National Oceanic and Atmospheric Administration

CREWS Standard (CREWS-STD) buoys are equipped to measure sea surface water temperature and conductivity (Sea-Bird Model SBE37-SM, Sea-Bird Electronics, Inc., www.seabird.com) at 1 m (nominal) below the water line and air temperature (R.M Young Model 41342); barometric pressure (Heise DXD and wind vectors (Vaisala WAS425A) at 2 m (nominal) above the water line. A compass (KVH C100 SE-25) is used in the calculation of wind direction and a GPS system provides geolocation.

Tags:

Modified: 2025-04-21

NOAA Coral Reef Watch Larval Connectivity, Florida Reef Tract

Data provided by  National Oceanic and Atmospheric Administration

Climate change threatens even the best-protected and most remote reefs. Reef recovery following catastrophic disturbance usually requires disturbed sites be reseeded from upstream reefs. Recent research (McClanahan et al., 2012) assessed connectivity as an important resilience factor, which although difficult to measure, is a high priority for management of coral reef ecosystems. The products discussed herein identify reefs that act as “sources” and/or “sinks” along the Florida Reef Tract to inform reef management strategies.

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Modified: 2025-04-21

NOAA Coral Reef Watch Larval Connectivity, Hawaiian Archipelago (and Johnston Atoll)

Data provided by  National Oceanic and Atmospheric Administration

Climate change threatens even the best-protected and most remote reefs. Reef recovery following catastrophic disturbance usually requires disturbed sites be reseeded from upstream reefs. Recent research (McClanahan et al., 2012) assessed connectivity as an important resilience factor, which although difficult to measure, is a high priority for management of coral reef ecosystems. The products described herein identify reefs that act as “sources” and/or “sinks” in the Hawaiian Archipelago (and Johnston Atoll) to inform reef management strategies.

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Modified: 2025-04-21

Seawater Temperature and Salinity Moored Time-Series Records, Collected During 2010 and 2011 in Vieques Sound and Virgin Passage (NODC Accession 0088063)

Data provided by  National Oceanic and Atmospheric Administration

Sea-Bird SBE37SM MicroCat Conductivity/Temperature (CT) recorders were deployed between March 2010 and April 2011 on shallow water moorings located in Vieques Sound, Puerto Rico, and Virgin Passage USVI. The recovered temperature, conductivity, and salinity (derived from temperature and conductivity) time-series data are presented here in an ACII format.

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Modified: 2025-04-21

Klawock Lagoon, Alaska Benthic Habitats 2011 Geodatabase

Data provided by  National Oceanic and Atmospheric Administration

The Klawock River on Alaska's Prince of Wales Island drains a 29,061 acre watershed with 132 miles of streambed habitat supporting seven salmon and trout species. Traditionally the river and lagoon supported salmon harvests exceeding 30,000 fish annually. The salmon fishery is an important economic factor and food source in the Klawock area. It is also an important cultural resource to local inhabitants. In 1964 a causeway was constructed blocking access to the lagoon from adjacent Klawock Bay. This has resulted in dramatic decreases in salmon harvests.

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Modified: 2025-04-21

Klawock Lagoon, Alaska Benthic Habitats 2011 Geoform

Data provided by  National Oceanic and Atmospheric Administration

The Klawock River on Alaska's Prince of Wales Island drains a 29,061 acre watershed with 132 miles of streambed habitat supporting seven salmon and trout species. Traditionally the river and lagoon supported salmon harvests exceeding 30,000 fish annually. The salmon fishery is an important economic factor and food source in the Klawock area. It is also an important cultural resource to local inhabitants. In 1964 a causeway was constructed blocking access to the lagoon from adjacent Klawock Bay. This has resulted in dramatic decreases in salmon harvests.

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Modified: 2025-04-21

Klawock Lagoon, Alaska Benthic Habitats 2011 Substrate

Data provided by  National Oceanic and Atmospheric Administration

The Klawock River on Alaska's Prince of Wales Island drains a 29,061 acre watershed with 132 miles of streambed habitat supporting seven salmon and trout species. Traditionally the river and lagoon supported salmon harvests exceeding 30,000 fish annually. The salmon fishery is an important economic factor and food source in the Klawock area. It is also an important cultural resource to local inhabitants. In 1964 a causeway was constructed blocking access to the lagoon from adjacent Klawock Bay. This has resulted in dramatic decreases in salmon harvests.

Tags:

Modified: 2025-04-21