AndreaBozzo/ceres-open-data-index huggingface dataset:
NOAA/WDS Paleoclimatology - Cosford et al. 2008 Xiangshui, Yaoba Don Caves Glacial Isotope Data

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Cave. The data include parameters of speleothems with a geographic location of China, Eastern Asia. The time period coverage is from 49911 to 19050 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: asia, carbon isotopes, cave deposits, china, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, eastern asia, land records, latitude 25.25, latitude 28.8, longitude 109.833, longitude 110.916, material: calcium carbonate, material: null, national centers for environmental information, nesdis, noaa, oxygen isotopes, paleoclimate, paleoclimate indicators, speleothems, u.s. department of commerce, what: age, what: delta 13c, what: delta 18o, what: depth, xiangshui cave, yaoba don cave
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Meko - Walnut Canyon - PIPO - ITRDB AZ592

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Tree Ring. The data include parameters of tree ring with a geographic location of Arizona, United States Of America. The time period coverage is from 422 to -60 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: arizona, biological records, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, land records, latitude 35.17, longitude -111.52, material: null, national centers for environmental information, nesdis, noaa, north america, paleoclimate, paleoclimate indicators, pinus ponderosa douglas ex c. lawson, pipo, ponderosa pine, tree ring, tree rings, tree-ring, u.s. department of commerce, united states of america, walnut canyon, western yellow pine, what: age, what: number of samples, what: total ring width, what: tree ring standardized growth index, width
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Dunwiddie - Okiwi - PHTR - ITRDB NEWZ015

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Tree Ring. The data include parameters of tree ring with a geographic location of New Zealand. The time period coverage is from 226 to -26 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: australia/new zealand, biological records, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, land records, latitude -41.12, longitude 173.67, material: null, national centers for environmental information, nesdis, new zealand, noaa, okiwi, paleoclimate, paleoclimate indicators, phtr, phyllocladus trichomanoides d. don, tanekaha, tree ring, tree rings, tree-ring, u.s. department of commerce, what: age, what: number of samples, what: total ring width, what: tree ring standardized growth index, width
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Kelly fire data from Chopper Lake, Yukon Flats, Alaska - IMPD USCPL008

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Fire. The data include parameters of fire history|paleolimnology with a geographic location of Alaska, United States Of America. The time period coverage is from 1561 to -58 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: alaska, arctic, charcoal sediment, chopper lake, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, fire history, fire history|paleolimnology, land records, latitude 66.00225, longitude -146.27532, material: null, material: sediment, material: wet sediment, medieval climate anomaly (mca), national centers for environmental information, nesdis, noaa, north america, paleoclimate, paleoclimate indicators, u.s. department of commerce, united states of america, what: age at sample end, what: age at sample start, what: charcoal, what: depth at sample end, what: depth at sample start, what: magnetic susceptibility, what: volume
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Meko - Jackson Meadow Reservoir - JUOC - CA631, PAGES North America 2K Version

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Tree Ring. The data include parameters of tree-ring (width) with a geographic location of California, United States Of America. The time period coverage is from 750 to -37 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: biological records, california, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, jackson meadow reservoir, juniperus occidentalis hook., juoc, land records, latitude 39.52, longitude -120.55, national centers for environmental information, nesdis, noaa, north america, pages 2k network, pages namerica 2k, paleoclimate, paleoclimate indicators, tree rings, tree-ring, u.s. department of commerce, united states of america, western juniper, width
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
Sea Level Rise: American Samoa: High-Tide Flooding: 2100 Intermediate-Low Scenario

This high-tide flooding layer provides a prediction of future sea level rise (SLR) inundation and was produced using a passive flooding model, often referred to as a "bathtub" model. It provides an assessment of flooded areas according to a specific water level. These water levels are determined using projections from the U.S. Interagency Task Force (ITF) (Sweet et al., 2022) in combination with land subsidence projections modeled by Han et al. (2019). The latter is included only for Tutuila, Aunuu, and Manua Islands (Ofu, Olosega, and Tau). In contrast, SLR projections for Swains Island and Rose Atoll only include the climate-related processes (ITF). The projections are modeled following both scenarios and time. The five scenarios range from low to high depending on the amount of greenhouse gases emissions, while time is divided by decade from 2030 to 2100.

We apply this model to the 2022 National Geodetic Survey (NGS) lidar DEM for American Samoa with 1-meter resolution. The DEM was leveled from NAD83 (PA11) to mean sea level at 0 m (MSL=0) in 2005. The adjustment of the DEM may lead to inaccuracies due to the lack of historic information. It is also important to acknowledge that any inaccuracies in the DEM will lead to inaccuracies in the flooding estimates.

In the 2100 intermediate-low scenario represented here, the modeled water level is 85 cm (48 cm for Rose and Swains). In this scenario, world-wide society limits increase of emissions, and sea level rises without reaching any tipping points, i.e. large and sudden changes such as a rapid increase in ice sheets melting. It is recommended to use this scenario only for planning construction of non-critical infrastructure that owners can afford to lose, such as a beach "fale".

Flood depth is provided in centimeters above the 2005 mean higher high water (MHHW) tide level.

It is essential to emphasize that the passive flooding model used to produce this data layer does not include the effects of waves on flooding. As a result, the extent and impacts of future flooding under high-wave conditions are not represented, which should be accounted for in planning efforts. In addition, the DEM is assumed to be unchanged as sea level rises, but in fact there will be erosion and changes in the shape of the land surface, and continued subsidence. This also must be considered, and it is best practice to consider any flooding extent or depth represented in this data layer as a best-case scenario, with the effects of dynamic shoreline processes leading to greater flood extent and depth than presented.

Tags: american samoa, atmospheric/ocean indicators, aunuu, climate indicators, coastal processes, earth science, environmental impacts, floods, human dimensions, inundation, manua, natural hazards, ocean, oceans, ofu, olosega, pacific islands ocean observing system, pacific ocean, pacioos, polynesia, rose atoll, sea level rise, south pacific ocean, swains, tau, tutuila
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
Photosynthetically Active Radiation (PAR) Standard Deviation of Long-term Mean, 2003-2018 - American Samoa

Solar irradiance is one of the most important factors influencing coral reefs. As a majority of their nutrients are obtained from symbiotic photosynthesizing organisms, reef-building corals need sunlight as a fundamental source of energy. Seasonally low irradiance at high latitudes may be linked to reduced growth rates in corals and may limit reef calcification to shallower depths than that observed at lower latitudes. However, high levels of irradiance can lead to light-induced damage, production of free radicals, and in combination with increased temperatures, can exacerbate coral bleaching. Irradiance is here represented by PAR (photosynthetically active radiation), which is the spectrum of light that is important for photosynthesis. This layer represents the standard deviation of the 8-day time series of PAR (mol/m2/day) from 2003-2018.

Data for PAR for the time period 2003-2018 were obtained from the Moderate Resolution Imaging Spectroradiometer (MODIS) Aqua satellite instrument from the NASA OceanColor website as 8-day 4-km composites.

The standard deviation of the long-term mean of PAR was calculated by taking the standard deviation over all 8-day data from 2003-2018 for each pixel. A quality control mask was applied to remove spurious data associated with shallow water, following Gove et al., 2013. Nearshore map pixels with no data were filled with values from the nearest neighboring valid offshore pixel by using a grid of points and the Near Analysis tool in ArcGIS then converting points to raster.

Data source: https://oceanwatch.pifsc.noaa.gov/erddap/griddap/aqua_par_8d_2018_0.graph

Tags: american samoa, aquatic ecosystems, biosphere, coastal areas, coastal processes, coral reef, coral reefs, earth science, ecosystems, human dimensions, human settlements, manua, marine ecosystems, ocean, ocean optics, oceans, ofu, olosega, pacific islands ocean observing system, pacific ocean, pacioos, photosynthetically active radiation, polynesia, reef, reef habitat, rose atoll, south pacific ocean, swains, tau, tutuila, vegetation
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
Commercial Harbors - Hawaii

Displays the locations of commercial harbors for the State of Hawaii. Commercial harbors and ports are harbors in which docks are provided with cargo-handling facilities.

Tags: central pacific ocean, continent, earth science, harbors, hawaii, hawaiian islands, human dimensions, infrastructure, north america, ocean, pacific islands ocean observing system, pacific ocean, pacioos, transportation, united states of america
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
Sea Level Rise: American Samoa: High-Tide Flooding: 2040 High Scenario

This high-tide flooding layer provides a prediction of future sea level rise (SLR) inundation and was produced using a passive flooding model, often referred to as a "bathtub" model. It provides an assessment of flooded areas according to a specific water level. These water levels are determined using projections from the U.S. Interagency Task Force (ITF) (Sweet et al., 2022) in combination with land subsidence projections modeled by Han et al. (2019). The latter is included only for Tutuila, Aunuu, and Manua Islands (Ofu, Olosega, and Tau). In contrast, SLR projections for Swains Island and Rose Atoll only include the climate-related processes (ITF). The projections are modeled following both scenarios and time. The five scenarios range from low to high depending on the amount of greenhouse gases emissions, while time is divided by decade from 2030 to 2100.

We apply this model to the 2022 National Geodetic Survey (NGS) lidar DEM for American Samoa with 1-meter resolution. The DEM was leveled from NAD83 (PA11) to mean sea level at 0 m (MSL=0) in 2005. The adjustment of the DEM may lead to inaccuracies due to the lack of historic information. It is also important to acknowledge that any inaccuracies in the DEM will lead to inaccuracies in the flooding estimates.

In the 2040 high scenario represented here, the modeled water level is 51 cm (19 cm for Rose and Swains). In this scenario, world-wide society continues to increase emissions. Tipping points (large and sudden changes) are triggered, and worst-case possibilities arise. It is recommended using this scenario for planning construction of infrastructure with highly critical use and longer lifespans, such as a new hospital.

Flood depth is provided in centimeters above the 2005 mean higher high water (MHHW) tide level.

It is essential to emphasize that the passive flooding model used to produce this data layer does not include the effects of waves on flooding. As a result, the extent and impacts of future flooding under high-wave conditions are not represented, which should be accounted for in planning efforts. In addition, the DEM is assumed to be unchanged as sea level rises, but in fact there will be erosion and changes in the shape of the land surface, and continued subsidence. This also must be considered, and it is best practice to consider any flooding extent or depth represented in this data layer as a best-case scenario, with the effects of dynamic shoreline processes leading to greater flood extent and depth than presented.

Tags: american samoa, atmospheric/ocean indicators, aunuu, climate indicators, coastal processes, earth science, environmental impacts, floods, human dimensions, inundation, manua, natural hazards, ocean, oceans, ofu, olosega, pacific islands ocean observing system, pacific ocean, pacioos, polynesia, rose atoll, sea level rise, south pacific ocean, swains, tau, tutuila
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
Sea Level Rise: American Samoa: High-Tide Flooding: 2050 Intermediate-Low Scenario

This high-tide flooding layer provides a prediction of future sea level rise (SLR) inundation and was produced using a passive flooding model, often referred to as a "bathtub" model. It provides an assessment of flooded areas according to a specific water level. These water levels are determined using projections from the U.S. Interagency Task Force (ITF) (Sweet et al., 2022) in combination with land subsidence projections modeled by Han et al. (2019). The latter is included only for Tutuila, Aunuu, and Manua Islands (Ofu, Olosega, and Tau). In contrast, SLR projections for Swains Island and Rose Atoll only include the climate-related processes (ITF). The projections are modeled following both scenarios and time. The five scenarios range from low to high depending on the amount of greenhouse gases emissions, while time is divided by decade from 2030 to 2100.

We apply this model to the 2022 National Geodetic Survey (NGS) lidar DEM for American Samoa with 1-meter resolution. The DEM was leveled from NAD83 (PA11) to mean sea level at 0 m (MSL=0) in 2005. The adjustment of the DEM may lead to inaccuracies due to the lack of historic information. It is also important to acknowledge that any inaccuracies in the DEM will lead to inaccuracies in the flooding estimates.

In the 2050 intermediate-low scenario represented here, the modeled water level is 49 cm (16 cm for Rose and Swains). In this scenario, world-wide society limits increase of emissions, and sea level rises without reaching any tipping points, i.e. large and sudden changes such as a rapid increase in ice sheets melting. It is recommended to use this scenario only for planning construction of non-critical infrastructure that owners can afford to lose, such as a beach "fale".

Flood depth is provided in centimeters above the 2005 mean higher high water (MHHW) tide level.

It is essential to emphasize that the passive flooding model used to produce this data layer does not include the effects of waves on flooding. As a result, the extent and impacts of future flooding under high-wave conditions are not represented, which should be accounted for in planning efforts. In addition, the DEM is assumed to be unchanged as sea level rises, but in fact there will be erosion and changes in the shape of the land surface, and continued subsidence. This also must be considered, and it is best practice to consider any flooding extent or depth represented in this data layer as a best-case scenario, with the effects of dynamic shoreline processes leading to greater flood extent and depth than presented.

Tags: american samoa, atmospheric/ocean indicators, aunuu, climate indicators, coastal processes, earth science, environmental impacts, floods, human dimensions, inundation, manua, natural hazards, ocean, oceans, ofu, olosega, pacific islands ocean observing system, pacific ocean, pacioos, polynesia, rose atoll, sea level rise, south pacific ocean, swains, tau, tutuila
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Baisan fire data from Rose Canyon Upper - IMPD USRCU001

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Fire. The data include parameters of fire history|tree ring with a geographic location of Arizona, United States Of America. The time period coverage is from 473 to -45 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: arizona, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, fire history, fire history|tree ring, fire scar dates, land records, latitude 32.39526, longitude -110.689, material: null, material: wood, national centers for environmental information, nesdis, noaa, north america, paleoclimate, paleoclimate indicators, rose canyon upper, u.s. department of commerce, united states of america, unkn, unknown, what: age, what: tree demographic and injury and fire event code
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Grissino-Mayer fire data from Cerro Bandera North - IMPD USCBN001

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Fire. The data include parameters of fire history|tree ring with a geographic location of New Mexico, United States Of America. The time period coverage is from 589 to -43 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: cerro bandera north, climate indicators, continent, doc/noaa/nesdis/ncei, earth science, fire history, fire history|tree ring, fire scar dates, land records, latitude 35, longitude -108.1, material: null, material: wood, national centers for environmental information, nesdis, new mexico, noaa, north america, paleoclimate, paleoclimate indicators, pinus ponderosa douglas ex c. lawson, pipo, ponderosa pine, u.s. department of commerce, united states of america, western yellow pine, what: age, what: tree demographic and injury and fire event code
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
NOAA/WDS Paleoclimatology - Dunwiddie - Manapouri Dam - DABI - ITRDB NEWZ010

This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Tree Ring. The data include parameters of tree ring with a geographic location of New Zealand. The time period coverage is from 383 to -26 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data.

Tags: australia/new zealand, biological records, climate indicators, continent, dabi, dacrydium biforme (hook.) pilg. = halocarpus biformis (hook.) quinn = halocarpus biformis hook., doc/noaa/nesdis/ncei, earth science, land records, latitude -45.53, longitude 167.3, manapouri dam, material: null, national centers for environmental information, nesdis, new zealand, noaa, pages 2k network, pages australasia 2k, paleoclimate, paleoclimate indicators, pink pine, tree ring, tree rings, tree-ring, u.s. department of commerce, what: age, what: number of samples, what: total ring width, what: tree ring standardized growth index, width
Organization: National Oceanic and Atmospheric Administration, Department of Commerce
EK80 Water Column Sonar Data Collected During W00714

Survey W00714 was conducted July 13-16, 2023 by NOAAâs Office of Coast Survey (OCS) in collaboration with academic partners. The partnership provided opportunities for undergraduate and graduate students to gain operational skills and proficiency in support of the development and long-range mission of hydrography. The primary objective of this seafloor mapping project was to collect multibeam bathymetry, acoustic backscatter, and water column data for use in updating NOAA's nautical charting products.

Tags: acoustic scattering, acoustic sounders, aquatic ecosystems, aquatic sciences, bathymetry, bathymetry/seafloor topography, benthic, biosphere, doc/noaa/nesdis/ncei, doc/noaa/nesdis/ngdc, earth science, ecosystems, fisheries, in situ/laboratory instruments, marine ecosystems, national centers for environmental information, national geophysical data center, nesdis, noaa, north atlantic ocean, ocean acoustics, oceans, pelagic, profilers/sounders, seafloor topography, u.s. department of commerce, vertical location, water column, water column mapping system, wcms
Organization: National Oceanic and Atmospheric Administration, Department of Commerce