The Boundaries and Remote Sensing Classification Datasets on Large Wetlands of International
Importance in 2001 and 2013
Zhang, H. Y.1 Niu, Z. G.1* Xu, P. P.1 Chen, Y. F.1 Hu, S. J.1 Gong, N.2
1. State Key Laboratory of Remote Sensing Science, Institute of Remote Sensing and Digital Earth,
Chinese Academy of Sciences, Beijing 100101, China??
2. Department of Resources and Environment, Shandong Agricultural University, Tai’an 271018, China
Abstract: Wetland is one of the ecosystems with the highest biodiversity and productivity in the world. In this paper, we developed a dataset of 100 large Wetlands of International Importance (the “Ramsar Sites”), which was developed by the data integration and mining from the World Database on Protected Areas (WDPA) and remote sensing images, expecially the high resolution imagery provided on the Google Earth and the Tianditu platforms. Each site covers at least an area of 200,000 hm2. Based on the Moderate Resolution Imaging Spectro radiometer (MODIS) 16-day composite products MOD13Q1 of these sites in 2001 and 2013, we applied the Savitzky-Golay filtering and time series reconstruction algorithms to Normalized Difference Vegetation Index (NDVI) data. The method of the Support Vector Machine (SVM) classifier was used to classify and map wetlands of these Ramsar sites. The time series data based wetland classification results were compared with high resolution remote sensing imagery and the relevant literatures. This method is more advantageous than single temporal imagery based wetland monitoring technique. The dataset consists of three components which are saved as .shp and .kmz file formats. The total data size is 102 MB in compressed file format.
Keywords: wetlands; boundary; remote sensing classification; wetland mapping; Ramsar sites
1 Introduction
Wetland is one of the ecosystems with the highest biodiversity and productivity in the world[1]. In recent years, large scale wetland monitoring and mapping emerged as a hot research topic and has been attracting great attention of many scholars because of its ecological significance. To understand the spatio-temporal change characteristics of wetland ecosystem is the key component of global change research[2]. The fast development of remote sensing technique provides an objective means to global wetlands monitoring research. The remotely sensed time series data play an irreplaceable role in the research of wetland changes in the growth cycle or in a calendar year of wetland vegetation[3]. It is the main data source of the remotely sensed monitoring on large wetlands of international importance at the global scale of this paper. Along with our related scientific reports published, we make this dataset available for public use.
2 Metadata of Dataset
The metadata of the boundaries and remote sensing classification datasets on large wetlands of international importance in 2001 and 2013 is summarized in Table 1[4]. It includes the dataset full name, short name, authors, year of the dataset, temporal resolution, spatial resolution, data format, data size, data files, data publisher, and data sharing policy, etc.
Table 1 Summary of the RamsarSites_Top100_WetlandCover_2001/2013 metadata.
Items
|
Description
|
Dataset full name
|
The wetland cover datasets on the large wetlands of international importance in 2001 and 2013 by remote sensing data integration
|
Dataset short name
|
RamsarSites_Top100_WetlandCover_2001/2013
|
Authors
|
Zhang, H. Y. L-4985-2016, Institute of Remote Sensing and Digital Earth, CAS, zhanghy@ radi.ac.cn
Niu, Z. G. L-4829-2016, Institute of Remote Sensing and Digital Earth, CAS, niuzg@ra di.ac.cn
Xu, P. P. L-5064-2016, Institute of Remote Sensing and Digital Earth, CAS, 25486400 46 @qq. com
Chen, Y. F. L-5003-2016, Institute of Remote Sensing and Digital Earth, CAS, 935836745 @qq.com
Hu, S. J. L-6142-2016, Institute of Remote Sensing and Digital Earth, CAS, husj1989@y eah.net
Gong, N. L-6422-2016, Shandong Agricultural University, gongningbaobao@126.com
|
Geographic region
|
100 large wetlands of international importance in the world, distributed in different continents
|
Year
|
2001, 2013
|
Temporal resolution
|
Yearly
|
Spatial resolution
|
250 m
|
Data format
|
.kmz, .shp
|
Data size
|
1.54 MB in .kmz format. 100 MB in compressed
|
Data files
|
The dataset consists of three files[4]. They are as follows.
1) Top100_boundary.kmz.zip. This is the boundaries of 100 large wetlands of international importance in the world. It is stored in a .kmz file applicable to Google Earth, and the data size is 1.54 MB
2) Ramsar2001.rar. This is the remotely sensed classification results of these wetlands in 2001. Its data size is 51 MB
3) Ramsar2013.rar. This is the remotely sensed classification results of these wetlands in 2013. Its data size is 49.6 MB
Note: The classification results, Ramsar2001.rar and Ramsar2013.rar, are stored as ArcGIS shapefile vector format. Each vector file includes seven fields: (1) Area refers to the area of each patch in square meters; (2) RSN stands for Ramsar Site No., namely Ramsar number or the number of wetlands of international importance; (3) Lev3 indicates wetland code of that patch in the classification system[4] (Table 2); (4) the fields Name_EN and Name_CN refer to the English names and the Chinese names of the Ramsar sites respectively; and (5) the fields Country_EN and Country_CN respectively stand for the English names and the Chinese names of the country where the Ramsar sites lie in
|
Foundation(s)
|
National Natural Science Foundation of China (41271423)
|
Data publisher
|
Global Change Research Data Publishing & Repository, http://www.geodoi.ac.cn
|
(To be continued on the next page)
|
(Continued)
|
Items
|
Description
|
Address
|
No. 11A, Datun Road, Chaoyang District, Beijing 100101, China
|
Data sharing policy
|
Data from the Global Change Research Data Publishing & Repository includes metadata, datasets (data products), and publications (in this case, in the Journal of Global Change Data & Discovery). Data sharing policy includes: (1) Data are openly available and can be free downloaded via the Internet; (2) End users are encouraged to use Data subject to citation; (3) Users, who are by definition also value-added service providers, are welcome to redistribute Data subject to written permission from the GCdataPR Editorial Office and the issuance of a Data redistribution license; and (4) If Data are used to compile new datasets, the ‘ten per cent principal’ should be followed such that Data records utilized should not surpass 10% of the new dataset contents, while sources should be clearly noted in suitable places in the new dataset[5]
|
3 Methods
3.1 The Objective and Indicators of Wetland Monitoring by Remote Sensing
Based on some principles such as wetlands with an area larger than 200,000 hm2, with established geographic extent and map information, 100 wetlands of international importance all over the world distributed at different ecological-climatic zones and continents were selected from the database of Ramsar sites (https://rsis.ramsar.org/) (Figure 1).
Figure 1 Spatial distribution of large wetlands
of international importance
|
Indices for monitoring large wetlands of international importance mainly include the types and the area of land cover (Table 2). The conversion between wetlands and non-wetlands, the conversion in different wetland types and the changes on the area of different types, were used as important indicators to eva-
luate the ecological and environmental conditions of the wetlands. In general, if wetlands are converted into non-wetlands, or natural wetlands are converted into artificial wetlands, they usually lead to a deteriorated environmental condition and pose some threats to wetland biodiversity conservation. On the contrary, it often causes healthy development on the wetland environments.
3.2 Methodology of Wetland Boundaries and Classification Dataset Development
Most of the wetland boundaries were delineated by reference to the scanned paper maps published on the Ramsar website (https://rsis.ramsar.org/. Retrieved on July 23, 2014)[6]. Another small part of them were derived from World Database on Protected Areas (https://www.iucn.org/; http://www.protectedplanet.net/. Retrieved on July 23, 2014) and the other products of literature and document. The maps were georeferenced in ArcGIS. Because there are many differences of wetland management and monitoring techniques in each country, some inconsistencies of the boundaries often occur in such occasion. Therefore we
made modification and verification by using high resolution remote sensing images on Google Earth platform, based on the physiographic forms of wetlands such as walking along rivers, roads, and the ridge lines. The MODIS product MOD13Q1 (16-day composite, 250 m)
Table 2 Land cover classification system adopted in remote sensing based mapping
on wetlands of international importance
Level 1
|
Level 2
|
Level 3
|
Code
|
Characteristics of time series NDVI
|
Definition or spatial distribution characteristics
|
Wetlands
|
Water
|
11
|
NDVI ≤ 0.1
|
Including rivers, lakes, estuarine wa ter, reservoirs and urban entertainment landscape, wastewater treatment plant, etc. It mainly refers to permanent water body
|
Forested/shrub-dominated wetlands
|
Forested/shrub-
dominated wetlands (evergreen)
|
121
|
NDVI ≥ 0.4. There is slight amplitude of variation on NDVI in a year
|
Including the forested/shrub-domin ated wetlands with evergreen vegetation located at the inland and coastal zone
|
Forested/shrub-
do min ated wetlands (deciduous)
|
122
|
NDVI ≥ 0.3. It presents a pattern of periodicity
|
Including the forested/shrub- dominated wetlands with deciduous vegetation located at the inland and coastal zone
|
Marshes
|
Permanent marshes
|
131
|
0.1 ≤ NDVI ≤ 0.5. There is a relative slight amplitude of variation on NDVI in a year. In high- water season, there may be minus value of NDVI
|
Wetlands with oversaturated soil and permanently flooded herbaceous plants
|
Seasonal marshes
|
132
|
0.1 ≤ NDVI ≤ 0.5. There is a periodic pattern of NDVI in a year. In high-water season,
NDVI < 0
|
Herbaceous marshes flooded regularly or seasonally in leaf-on season
|
Flooded flats/Intertidal zone / Estuarine deltas
|
14
|
NDVI ≤ 0.2. In high-water season,
NDVI < 0
|
They refer to inundated periodically and oversaturated soils distributed near lakes, rivers and estuary, with the vegetation coverage lower than 30%. They are often not covered with open water
|
Paddy fields
|
15
|
NDVI < 0, at the early stage of crop growth. There is a steep decreasing trend of NDVI after crops harvesting
|
Arable land used for growing rice
|
Tundra wetlands
|
16
|
In leaf-on season, NDVI < 0.6. They are usually distributed at high latitudes
|
|
Non-
wetlands
|
Snow
|
21
|
|
Perennial snow
|
Natural
vegetation
|
Forests/Scrublands
|
22
|
In the leaf-on season, NDVI>0.5
|
Forests and scrublands
|
Grasslands
|
23
|
In the leaf-on season,
0.3 ≤NDVI≤0.6
|
|
Construction / Barren lands
|
24
|
0≤NDVI≤0.2
|
Including artificial construction such as buildings, roads, etc. and other forms of barren lands, e.g., rocks, barren sands
|
Drylands
|
25
|
The occurrence of the slow growth and the steep drop-off of the NDVI value in a calendar year
|
Farms cultivated with dry-land crops as a result of their scarcity of water
|
Cloud cover
|
32
|
|
These regions are covered by clouds
|
Ocean
|
33
|
|
|
in 2001 and 2013 downloaded from NASA (https://ladsweb.nascom.nasa.gov/data/) was used as the main data source. There are 23 periods of the images in each year. In this study, the images on the public service platform Tianditu (http://www.tianditu.com/map/index.html) powered by the National Geomatics Center of China (NGCC) and other geographic data were also used as auxiliary data. The Normalized Difference Vegetation Index (NDVI) can reflect the growth status of different vegetation types. By comparing the NDVI differences including the maximum, the minimum, and the range of annual NDVI, the emergence date of the positive NDVI value, and the growing season length, etc. between different vegetation types in the growth cycle or within a calendar year, and analyzing plants growth pattern[7], the accuracy of interpretation on different types of land cover types could be effectively improved. We applied Savitzky-Golay filtering to reconstruct NDVI time series dataset[8]. Based on the clustering results of time series data and the analysis on the features of different land cover types in high resolution remote sensing images, we collected 10-20 training samples for each type and used SVM classifier to delineate and map different types of wetlands. The minimum of the map unit is about 56.25 hm2 for 3×3 pixels. The main methods and the technical flow are described in Figure 2.
Figure 2 Flowchart for wetlands classification
|
4 Data Products
The dataset consists of three components, namely Top100_boundary kmz (1,470.14 KB), Ramsar2001.rar (52,245.46 KB) and Ramsar2013.rar (50,858.42 KB). They represent the boundaries of 100 large wetlands of international importance in the world, and the wetland classification results in 2001 and 2013, respectively (http://www.geodoi.ac.cn/WebEn/doi.aspx?
Id=243).
4.1 Statistics on Large Wetlands of International Importance
The total area of 100 large wetlands of international importance is 138,392,121.05 hm2. Okavango Delta System (Ramsar Site No.879), located in Botswana, ranks first. The statistical results are listed in Table 3.
Table 3 Statistics on large wetlands of international importance
Name of Ramsar Sites
|
Area (hm2)
|
Country
|
Ramsar Site No.
|
|
Okavango Delta System
|
6,703,463.94
|
Botswana
|
879
|
Queen Maud Gulf
|
6,263,006.27
|
Canada
|
246
|
Ngiri-Tumba-Maindombe
|
6,194,581.31
|
Democratic Republic of the Congo
|
1784
|
Plaines d’inondation des Bahr Aouk et Salamat
|
6,187,728.80
|
Chad
|
1621
|
Grands affluents
|
5,787,900.96
|
Republic of Congo
|
1742
|
Plaines d’inondation du Logone et les dépressions Toupouri
|
4,017,225.78
|
Chad
|
1560
|
Complejo de humedales del Abanico del río Pastaza
|
3,781,662.25
|
Peru
|
1174
|
Malagarasi-Muyovozi Wetlands
|
3,705,800.43
|
Tanzania
|
1024
|
Río Yata
|
3,448,554.92
|
Bolivia
|
2094
|
Palmar de las Islas y las Salinas de San José
|
3,434,589.67
|
Bolivia
|
1088
|
(To be continued on the next page)
|
(Continued)
|
Name of Ramsar Sites
|
Area (hm2)
|
Country
|
Ramsar Site No.
|
Delta Intérieur du Niger
|
3,143,537.63
|
Mali
|
1365
|
Río Blanco
|
2,909,863.42
|
Bolivia
|
2092
|
Plaine de Massenya
|
2,905,803.26
|
Chad
|
1839
|
Reentrancias Maranhenses
|
2,671,201.38
|
Brazil
|
640
|
Area between the Pura & Mokoritto Rivers
|
2,620,671.33
|
Russia
|
697
|
Sudd
|
2,470,516.39
|
South Sudan
|
1622
|
Gueltas et Oasis de l’Aïr
|
2,413,275.61
|
Niger
|
1501
|
Réserve Naturelle Nationale des Terres Australes Francaises
|
2,332,885.13
|
French
|
1837
|
Polar Bear Provincial Park
|
2,231,833.08
|
Canada
|
360
|
Pacaya-Samiria
|
2,194,600.24
|
Peru
|
546
|
Coongie Lakes
|
2,142,810.22
|
Australia
|
376
|
Río Matos
|
2,116,721.12
|
Bolivia
|
2093
|
Kakadu National Park
|
1,939,734.28
|
Australia
|
204
|
Parapolsky Dol
|
1,826,613.22
|
Russia
|
693
|
Baixada Maranhense Environmental Protection Area
|
1,811,854.16
|
Brazil
|
1020
|
Los Lípez
|
1,729,203.22
|
Bolivia
|
489
|
Lake Niassa and its Coastal Zone
|
1,697,149.57
|
Mozambique
|
1964
|
Partie tchadienne du lac Tchad
|
1,686,175.47
|
Chad
|
1134
|
Whooping Crane Summer Range
|
1,616,992.61
|
Canada
|
240
|
Parc National du Banc d’Arguin
|
1,477,460.61
|
Mauritania
|
250
|
Suakin-Gulf of Agig
|
1,450,427.12
|
Sudan
|
1860
|
Site Ramsar Odzala Kokoua
|
1,385,476.02
|
Republic of Congo
|
2080
|
Lago Titicaca
|
1,366,536.56
|
Bolivia
|
959
|
Bañados del Río Dulce y Laguna de Mar Chiquita
|
1,351,673.35
|
Argentina
|
1176
|
Mamirauá
|
1,319,593.43
|
Brazil
|
623
|
Lagunas altoandinas y puneñas de Catamarca
|
1,311,834.01
|
Argentina
|
1865
|
Tobol-Ishim Forest-steppe
|
1,278,538.61
|
Russia
|
679
|
Gambie-Oundou-Liti
|
1,246,779.36
|
Guinea
|
1579
|
Volga Delta
|
1,199,249.85
|
Russia
|
111
|
Lagunas de Guanacache, Desaguadero y del Bebedero
|
1,157,839.02
|
Argentina
|
1012
|
Zambezi Delta
|
1,140,940.11
|
Mozambique
|
1391
|
Lagos Poopó y Uru Uru
|
1,136,273.65
|
Bolivia
|
1181
|
Archipel Bolama-Bijagós
|
1,065,174.91
|
Guinea-Bissau
|
2198
|
Ili River Delta and South Lake Balkhash
|
973,699.53
|
Kazakhstan
|
2020
|
Lake Uvs and its surrounding wetlands
|
885,360.38
|
Mongolia
|
1379
|
Har Us Nuur National Park
|
859,526.41
|
Mongolia
|
976
|
Dinder National Park
|
855,072.75
|
Sudan
|
1461
|
Alakol-Sasykkol Lakes System
|
784,807.01
|
Kazakhstan
|
1892
|
Dewey Soper Migratory Bird Sanctuary
|
782,498.00
|
Canada
|
249
|
Le Lac Alaotra: Les Zones Humides et Bassins Versants
|
781,472.69
|
Madagascar
|
1312
|
Everglades National Park
|
754,573.06
|
United States
|
374
|
Brekhovsky Islands in the Yenisei estuary
|
737,894.04
|
Russia
|
698
|
Área de Protección de Flora y Fauna Laguna de Términos
|
734,350.69
|
Mexico
|
1356
|
Rufiji-Mafia-Kilwa Marine Ramsar Site
|
734,194.39
|
Tanzania
|
1443
|
(To be continued on the next page)
|
(Continued)
|
Name of Ramsar Sites
|
Area (hm2)
|
Country
|
Ramsar Site No.
|
Dalai Lake National Nature Reserve, Inner Mongolia
|
733,235.89
|
China
|
1146
|
Sian Ka'an
|
655,727.26
|
Mexico
|
1329
|
Aydar-Arnasay Lakes system
|
636,595.85
|
Uzbekistan
|
1841
|
Isyk-Kul State Reserve with the Lake Isyk-Kul
|
629,536.18
|
Kyrgyzstan
|
1231
|
Chott El Jerid
|
616,315.19
|
Tunisia
|
1699
|
Lake Chad Wetlands in Nigeria
|
611,134.90
|
Nigeria
|
1749
|
Rio Sabinas
|
606,876.07
|
Mexico
|
1769
|
Eqalummiut Nunaat and Nassuttuup Nunaa
|
594,195.32
|
Denmark
|
386
|
Ilha do Bananal
|
592,910.39
|
Brazil
|
624
|
Site Ramsar du Complexe W
|
581,917.66
|
Benin
|
1668
|
Sangha-Nouabalé-Ndoki
|
552,358.22
|
Republic of Congo
|
1858
|
Wadden Sea
|
541,257.30
|
Netherlands
|
289
|
Cabo Orange National Park
|
523,199.02
|
Brazil
|
2190
|
Bafing-Falémé
|
522,191.82
|
Guinea
|
1719
|
Chott Ech Chergui
|
519,421.40
|
Algeria
|
1052
|
Bañados del Izozog y el río Parapetí
|
516,491.19
|
Bolivia
|
1087
|
Runn of Kutch
|
513,386.48
|
Pakistan
|
1285
|
Sundarbans Reserved Forest
|
499,921.44
|
Bangladesh
|
560
|
Upper Dvuobje
|
499,157.08
|
Russia
|
678
|
Jaaukanigás
|
491,725.87
|
Argentina
|
1112
|
Humedales Chaco
|
491,620.32
|
Argentina
|
1366
|
Schleswig-Holstein Wadden Sea and adjacent areas
|
481,776.92
|
Germany
|
537
|
Lake Sevan
|
474,652.91
|
Armenia
|
620
|
Lake Urmia [or Orumiyeh]
|
456,996.73
|
Iran
|
38
|
Danube Delta
|
451,407.18
|
Romania
|
521
|
Indus Delta
|
435,103.46
|
Pakistan
|
1284
|
Wasur National Park
|
411,337.03
|
Indonesia
|
1624
|
Chany Lakes
|
387,239.92
|
Russia
|
680
|
Tanjung Puting National Park
|
378,350.88
|
Indonesia
|
2192
|
Zones Humides du Littoral du Togo
|
368,011.51
|
Togo
|
1722
|
Shadegan Marshes & mudflats of Khor-al Amaya & Khor Musa
|
334,645.27
|
Iran
|
41
|
Turkmenbashy Bay
|
324,761.47
|
Turkmenistan
|
1855
|
Hopen
|
316,453.18
|
Norway
|
1957
|
Lesser Aral Sea and Delta of the Syrdarya River
|
313,371.18
|
Kazakhstan
|
2083
|
Bear Island
|
296,711.28
|
Norway
|
1966
|
Lemmenjoki National Park
|
285,550.79
|
Finland
|
1521
|
Lakes of the lower Turgay and Irgiz
|
263,261.44
|
Kazakhstan
|
108
|
Tengiz-Korgalzhyn Lake System
|
261,593.75
|
Kazakhstan
|
107
|
Gansu Gahai Wetlands Nature Reserve
|
247,747.47
|
China
|
1975
|
Etangs de la Champagne humide
|
241,348.36
|
France
|
514
|
Kama-Bakaldino Mires
|
223,709.33
|
Russia
|
670
|
Lake Khanka
|
192,382.13
|
Russia
|
112
|
Chott Melghir
|
192,282.62
|
Algeria
|
1296
|
Veselovskoye Reservoir
|
185,046.81
|
Russia
|
672
|
Petit Loango
|
150,542.08
|
Gabon
|
352
|
Old Crow Flats
|
31,461.26
|
Canada
|
244
|
|
|
|
|
|
|
4.2 Remote Sensing Classification Results on Large Wetland of International Importance in 2001 and 2013
Based on the remote sensing classification results on 100 large wetlands of international importance in 2001 and 2013, we calculate the subtotal area of different land cover types. The statistical results are shown in Table 4.
In 2001, the largest three wetland classes are forested/shrub-dominated wetlands (deciduous), seasonal marshes, and permanent marshes, respectively. Between 2001 and 2013, the total area of wetland reduced from 58,134,960 hm2 to 57,734,032 hm2, the big three losers were water, forested/shrub-dominated wetlands (deciduous), and tundra wetlands, respectively.
Table 4 Area of different land cover types in large wetlands of international importance
Code
|
Level 2
|
Level 3
|
Area (hm2)
|
2001
|
2013
|
Wetlands
|
58,134,960.36
|
57,734,032.42
|
11
|
Water
|
|
7,962,751.49
|
7,220,121.10
|
121
|
Forested/shrub-dominated wetlands
|
Forested/shrub-dominated wetlands (evergreen)
|
5,670,938.35
|
5,372,163.35
|
122
|
Forested/shrub-dominated wetlands (deciduous)
|
17,989,514.92
|
17,264,579.94
|
131
|
Marshes
|
Permanent marshes
|
8,852,939.87
|
9,019,623.32
|
132
|
Seasonal marshes
|
11,446,049.25
|
12,970,340.19
|
14
|
Flooded flats/Intertidal zone / Estuarine deltas
|
|
3,677,715.96
|
3,755,553.93
|
15
|
Paddy fields
|
|
161,536.44
|
118,356.86
|
16
|
Tundra wetlands
|
|
2,373,514.09
|
2,013,293.73
|
Non-wetlands
|
80,256,924.04
|
80,657,761.93
|
21
|
Snow
|
|
203,466.14
|
161,471.34
|
22
|
Natural vegetation
|
Forests/Scrublands
|
49,795,219.42
|
49,793,411.47
|
23
|
Grasslands
|
10,253,074.54
|
10,202,998.58
|
24
|
Construction / Barren lands
|
|
10,255,547.25
|
9,634,365.16
|
25
|
Drylands
|
|
2,071,076.67
|
3,200,432.37
|
32
|
Cloud cover
|
|
54,188.66
|
53,787.91
|
33
|
Ocean
|
|
7,624,351.36
|
7,611,295.11
|
5 Data Validation
Validation on the world’s large wetlands classification results accuracy was applied by
using high resolution remotely sensed images. We randomly selected 10 wetlands of international importance in different continents as the testing regions except for the Antarctic. About 2,386 validation samples randomly collected were interpreted based on high resolution images of China’s satellites GF-1, ZY-3. Accuracy of all land cover types was assessed. In general, the overall accuracy for all types is 88% and 89% in 2001 and 2013 respectively. And the Kappa coefficients are 0.86 and 0.87 respectively.
The dataset contains the boundaries of the world’s 100 large wetlands of international importance and wetland classification results on them in 2001 and 2013 based on 250 m spatial resolution, 16-day composite product MOD13Q1. It provides important reference data for research on global wetlands and climate change.
Author Contributions
Six coauthors were engaged in the design and development of the boundaries and remote sensing classification datasets on large wetlands of international importance in 2001 and 2013. Zhang, H. Y. and Niu, Z. G. participated in all the technological processes of the design and methodological development of boundaries extraction, data collection and processing, data analysis and validation, etc. Zhang, H. Y., Xu, P. P., Chen, Y. F., Hu, S. J. and Gong, N. took part in the boundaries extraction and wetlands classification. And the author list was arranged in their workload order. Zhang, H. Y. wrote this paper, and Niu, Z. G. was in charge of the paper proofreading, editing and revision.
Acknowledgements
We appreciate the National Geomatics Center of China, Google Earth, and the National Aeronautics and Space Administration (NASA), US for providing online public services of Tianditu, Google Earth and MODIS data.
References
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