Measured Quantity Community Instance
API endpoint that allows MeasuredQuantity of Communities to be viewed or edited.
GET /sms/cv/api/v1/measuredquantities-communities/603/?format=api
https://gravis.gfz-potsdam.de/gws", "note": "" }, "relationships": { "sampling_media": { "links": { "self": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/relationships/sampling_media?format=api", "related": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/sampling_media/?format=api" }, "data": { "type": "SamplingMedium", "id": "15" } }, "aggregation_type": { "links": { "self": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/relationships/aggregation_type?format=api", "related": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/aggregation_type/?format=api" }, "data": { "type": "AggregationType", "id": "1" } }, "root": { "links": { "self": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/relationships/root?format=api", "related": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/root/?format=api" }, "data": { "type": "MeasuredQuantity", "id": "398" } }, "community": { "links": { "self": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/relationships/community?format=api", "related": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/community/?format=api" }, "data": { "type": "Community", "id": "6" } } }, "links": { "self": "https://sms-cv.helmholtz.cloud/sms/cv/api/v1/measuredquantities-communities/603/?format=api" } } }{ "data": { "type": "MeasuredQuantityCommunity", "id": "603", "attributes": { "term": "Glacier mass uncertainty", "abbreviation": null, "definition": "Time-variable component of the uncertainty estimates for the filtered glacier mass anomalies; glacier mass change uncertainties are based on the inherited uncertainties from the glaciological and the geodetic input datasets and their variability, at a 95% confidence interval (1.96 std); uncertainty propagation considers the glaciated area of a grid cell and the number of independent observations; finally, to convert from specific mass balance uncertainties to water mass loss (Gt) and water height uncertainties (mm), an additional source of error related to the glacier area and area change rates are considered.", "provenance": null, "provenance_uri": "