- Title
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under R...
- Abstract
The data layers provided show current values for seawater temperature, pH, calcite and aragonite saturation (%), oxygen concentration, and particulate organic carbon (POC) flux to the seafloor at different depths (500, 1000, 2000, 3000, and 4000m) at the present day (1951-2000) and changes in these variables expected between 2041-2060 and 2081-2100 under different RCP scenarios. The data layers were generated following the methods described in Levin et al. (2020). In short, in 2019, we obtained the present day and future ocean projections for the different years which were compiled from all available data generated by Earth Systems Models as part of the Coupled Model Inter-comparison Project Phase 5 (CMIP5) to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. Three Earth System Models, including GFDL‐ESM‐2G, IPSL‐CM5A‐MR, and MPI‐ESM‐MR were collected and multi-model averages of temperature, pH, O2 , export production at 100-m depth (epc100), carbonat...
- License
- Creative Commons Attribution 4.0 International (CC BY 4.0)
-
+ This is a human-readable summary of (and not a substitute for) the license. Disclaimer.
+ You are free to:
+ Share — copy and redistribute the material in any medium or format
+ Adapt — remix, transform, and build upon the material
+ for any purpose, even commercially.
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+ Under the following terms:
+ Attribution — You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
+
+ No additional restrictions — You may not apply legal terms or technological measures that legally restrict others from doing anything the license permits.
+ Notices:
+ You do not have to comply with the license for elements of the material in the public domain or where your use is permitted by an applicable exception or limitation.
+ No warranties are given. The license may not give you all of the permissions necessary for your intended use. For example, other rights such as publicity, privacy, or moral rights may limit how you use the material.
+ For more info see https://creativecommons.org/licenses/by/4.0/. - Publication Date
- Jan. 28, 2023, 7:47 a.m.
- Type
- Raster Data
- Keywords
- Aragonite saturation Atlantic Ocean RCP2.6 RCP4.5 RCP8.5 Climate change data-layers GeoTIFF iAtlantic Integrated Assessment of Atlantic Marine Ecosystems in Space and Time O2 pH POC flux RCP26_pH_Difference_2081_2100_1951_2000 Temperature WCS
- Category
- geoscientificInformation
- Regions
- Global
- Approved
- Yes
- Published
- Yes
- Featured
- No
- Name
- Andrew.Sweetman
- Andrew.Sweetman@sams.ac.uk
- Position
- None
- Organization
- None
- Location
- Voice
- None
- Fax
- None
- Identification Image
-
- Spatial Extent
- ---
- Projection System
- EPSG:4326
- Extension x0
- -98.000000000000000
- Extension x1
- 20.000000000000000
- Extension y0
- -50.000000000000000
- Extension y1
- 66.500000000000000
- Restrictions
- CC-BY-4.0: Creative Commons Attribution 4.0 International
- Language
- English
- Temporal Extent
- Jan. 1, 1951, midnight - Dec. 31, 2100, midnight
- Data Quality
- The data set was checked for completeness, correctness, and consistency of metainformation. Validity of used methods was checked and - if applicable - precision and range of data.
- Supplemental Information
No information provided
- Name
- chihlinwei
- clwei@ntu.edu.tw
- Position
- None
- Organization
- None
- Location
- Voice
- None
- Fax
- None
- Link Online
- /layers/RCP26_pH_Difference_2081_2100_1951_2000:geonode:RCP26_pH_Difference_2081_2100_1951_2000
- Metadata Page
- /layers/RCP26_pH_Difference_2081_2100_1951_2000:geonode:RCP26_pH_Difference_2081_2100_1951_2000/metadata_detail
- Thumbnail
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.png
- Remote Thumbnail
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.png
- Legend
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.png
- GeoTIFF
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.geotiff
- GZIP
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.x-gzip
- PNG
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.png
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.pdf
- JPEG
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.jpg
- Original Dataset
- Modeled pH Difference between periods 2081 to 2100 minus 1951 to 2000 under RCP26 for the deep Atlantic Ocean.zip
- OGC WCS: geonode Service
- Geoservice OGC:WCS
- OGC WMS: geonode Service
- Geoservice OGC:WMS
- Name
- chihlinwei
- clwei@ntu.edu.tw
- Position
- None
- Organization
- None
- Location
- Voice
- None
- Fax
- None