Dataset:
Southeast Asia Tropical cyclone landfall database

dc.coverage.spatial Southeast Asia
dc.date.accessioned 2022-02-09T23:19:03Z
dc.date.available 2022-02-09T23:19:03Z
dc.date.issued 2022-02-09
dc.description.abstract This database includes four Tropical cyclone (TC) landfall datasets produced using the Regional Specialized Meteorological Center of Tokyo (TOKYO), China Meteorological Administration (CMA), Hong Kong Observatory (HKO), and Joint Typhoon Warning Center (JTWC) best track datasets. The database was used to investigate a 50-yr TC landfalling climatology in Southeast Asia (1970-2019). These datasets are at 30-min temporal and 0.25-degree spatial resolutions and stored in the Matlab ".m" file format. The column variable description of each dataset is as below. 1) id: Tropical cyclone identifier 2) name: Tropical cyclone name 3) syear: Forming year 4) obs: Time provided in Universal Time Coordinates (UTC). Format is YYYY-MM-DD_HH:mm:ss 5) lat: Latitude 6) lon: Longitude 7) v: Maximum wind speed (converted to 1-min wind speed in case the dataset is CMA, HKO, TOKYO) 8) hit_lat: Latitude of landfall 9) hit_lon: Longitude of landfall 10) hit_v: Intensity at landfall (defined by maximum wind speed converted to 1-min in case the dataset is CMA, HKO, TOKYO) 11) v_orig: Maximum wind speed provided by an agency 12) hit_v_orig: Intensity at landfall defined by maximum wind speed provided by an agency 13) hit_obs: Time of landfall 14) hit_times: Number of landfalls
dc.identifier.uri http://hdl.handle.net/1959.4/100077
dc.language English
dc.language.iso en
dc.rights CC-BY-NC
dc.rights.uri https://creativecommons.org/licenses/by-nc/4.0/
dc.subject.other Tropical cyclone
dc.subject.other Landfall
dc.subject.other Climatology
dc.title Southeast Asia Tropical cyclone landfall database
dc.type Dataset
dcterms.accessRights open access
dcterms.accrualMethod To generate this database, the Natural Earth coastline dataset (1:50 million) was used to define the Southeast Asia coastline. A landfall time was recorded whenever a TC crossed from water to land and an individual TC can make landfall multiple times by crossing land back to ocean, then back onto land. A condition of “at least 50 km in distance” between two consecutive landfalls was applied to subtract unrealistically inflated landfalls caused by the zigzag pattern of the coastlines.
dcterms.rightsHolder Thao Linh Tran
dspace.entity.type Dataset
unsw.accessRights.uri https://purl.org/coar/access_right/c_abf2
unsw.contributor.researchDataCreator Tran, Thao Linh
unsw.coverage.temporalFrom 1970-01-01
unsw.coverage.temporalText 1970 - 2019
unsw.coverage.temporalTo 2019-12-31
unsw.description.contact t.thaolinh@gmail.com
unsw.identifier.doi https://doi.org/10.26190/unsworks/1987
unsw.isPublicationRelatedToDataset https://doi.org/10.1029/2021JD036301
unsw.isPublicationRelatedToDataset Tropical Cyclone behaviour and impacts in Southeast Asia, historically and in the warming future
unsw.relation.faculty UNSW Canberra
unsw.relation.school School of Science
unsw.subject.fieldofresearchcode 3701 Atmospheric sciences
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