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Article: Construction of the 500-m Resolution Daily Global Surface Water Change Database (2001–2016)
Title | Construction of the 500-m Resolution Daily Global Surface Water Change Database (2001–2016) |
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Authors | |
Keywords | MODIS water water change water time series daily water mapping |
Issue Date | 2018 |
Citation | Water Resources Research, 2018, v. 54, n. 12, p. 10270-10292 How to Cite? |
Abstract | Surface water is the most dynamic land-cover type. Transitions between water and nonwater types (such as vegetation and ice) can happen momentarily. More frequent mapping is necessary to study the changing patterns of water. However, monitoring of long-term global water changes at high spatial resolution and in high temporal frequency is challenging. Here we report the generation of a daily global water map data set at 500-m resolution from 2001 to 2016 based on the daily reflectance time series from Moderate Resolution Imaging Spectroradiometer. Each single-date image is classified into three types: water, ice/snow, and land. Following temporal consistency check and spatial-temporal interpolation for missing data, we conducted a series of validation of the water data set. The producer's accuracy and user's accuracy are 94.61% and 93.57%, respectively, when checked with classification results derived from 30-m resolution Landsat images. Both the producer's accuracy and user's accuracy reached better than 90% when compared with manually interpreted large-sized sample units (≥1,000 m × 1,000 m) collected in a previous global land cover mapping project. Generally, the global inland water area reaches its maximum (~3.80 × 10 6 km 2 ) in September and minimum (~1.50 × 10 6 km 2 ) in February during an annual cycle. Short-duration water bodies, sea level rise effects, different types of rice field use can be detected from the daily water maps. The size distribution of global water bodies is also discussed from the perspective of the number of water bodies and the corresponding water area. In addition, the daily water maps can precisely reflect water freezing and help correct water areas with inconsistent cloud flags in the MOD09GA quality assessment layer. |
Persistent Identifier | http://hdl.handle.net/10722/296865 |
ISSN | 2023 Impact Factor: 4.6 2023 SCImago Journal Rankings: 1.574 |
ISI Accession Number ID |
DC Field | Value | Language |
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dc.contributor.author | Ji, Luyan | - |
dc.contributor.author | Gong, Peng | - |
dc.contributor.author | Wang, Jie | - |
dc.contributor.author | Shi, Jiancheng | - |
dc.contributor.author | Zhu, Zhiliang | - |
dc.date.accessioned | 2021-02-25T15:16:51Z | - |
dc.date.available | 2021-02-25T15:16:51Z | - |
dc.date.issued | 2018 | - |
dc.identifier.citation | Water Resources Research, 2018, v. 54, n. 12, p. 10270-10292 | - |
dc.identifier.issn | 0043-1397 | - |
dc.identifier.uri | http://hdl.handle.net/10722/296865 | - |
dc.description.abstract | Surface water is the most dynamic land-cover type. Transitions between water and nonwater types (such as vegetation and ice) can happen momentarily. More frequent mapping is necessary to study the changing patterns of water. However, monitoring of long-term global water changes at high spatial resolution and in high temporal frequency is challenging. Here we report the generation of a daily global water map data set at 500-m resolution from 2001 to 2016 based on the daily reflectance time series from Moderate Resolution Imaging Spectroradiometer. Each single-date image is classified into three types: water, ice/snow, and land. Following temporal consistency check and spatial-temporal interpolation for missing data, we conducted a series of validation of the water data set. The producer's accuracy and user's accuracy are 94.61% and 93.57%, respectively, when checked with classification results derived from 30-m resolution Landsat images. Both the producer's accuracy and user's accuracy reached better than 90% when compared with manually interpreted large-sized sample units (≥1,000 m × 1,000 m) collected in a previous global land cover mapping project. Generally, the global inland water area reaches its maximum (~3.80 × 10 6 km 2 ) in September and minimum (~1.50 × 10 6 km 2 ) in February during an annual cycle. Short-duration water bodies, sea level rise effects, different types of rice field use can be detected from the daily water maps. The size distribution of global water bodies is also discussed from the perspective of the number of water bodies and the corresponding water area. In addition, the daily water maps can precisely reflect water freezing and help correct water areas with inconsistent cloud flags in the MOD09GA quality assessment layer. | - |
dc.language | eng | - |
dc.relation.ispartof | Water Resources Research | - |
dc.rights | This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License. | - |
dc.subject | MODIS | - |
dc.subject | water | - |
dc.subject | water change | - |
dc.subject | water time series | - |
dc.subject | daily water mapping | - |
dc.title | Construction of the 500-m Resolution Daily Global Surface Water Change Database (2001–2016) | - |
dc.type | Article | - |
dc.description.nature | published_or_final_version | - |
dc.identifier.doi | 10.1029/2018WR023060 | - |
dc.identifier.scopus | eid_2-s2.0-85059070176 | - |
dc.identifier.volume | 54 | - |
dc.identifier.issue | 12 | - |
dc.identifier.spage | 10270 | - |
dc.identifier.epage | 10292 | - |
dc.identifier.eissn | 1944-7973 | - |
dc.identifier.isi | WOS:000456949300015 | - |
dc.identifier.issnl | 0043-1397 | - |