Matches in climatepub4-kg for { <https://climateKG.org/entity/3678d18c-9dca-4743-abc0-1442b4d438d2> ?p ?o ?g. }
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- 3678d18c-9dca-4743-abc0-1442b4d438d2 MeasuredAt 26d3953e-be79-46e4-b746-efb1983c3f5c @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 type Science_Keyword @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 type Variable @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 broader 09d00879-6d96-4df4-9f50-73bd761118d9 @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 broader 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 broader 7406a787-6ab6-429f-bc09-9a86d393e114 @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 broader 894f9116-ae3c-40b6-981d-5113de961710 @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 definition "Drought should be considered relative to some longterm average condition ofbalance between precipitation and evapotranspiration ET in a particular areaa condition often perceived as normal Common to all types of drought is thefact that they originate from a deficiency of precipitation that results inwater shortage for some activity or for some group It is also commonlyrecognized that other meteorological elements such as temperature wind andrelative humidity may aggravate the severity and impacts of drought in someinstances BRBR A Drought Advisory may report on drought occurring in a particular region" @default.
- 3678d18c-9dca-4743-abc0-1442b4d438d2 prefLabel "DROUGHT" @default.