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Development of the global dataset of Wetland Area and Dynamics for Methane Modeling (WAD2M)

Authors :
Z. Zhang
E. Fluet-Chouinard
K. Jensen
K. McDonald
G. Hugelius
T. Gumbricht
M. Carroll
C. Prigent
A. Bartsch
B. Poulter
University of Maryland [College Park]
University of Maryland System
Stanford University
City College of New York [CUNY] (CCNY)
City University of New York [New York] (CUNY)
California Institute of Technology (CALTECH)
Stockholm University
NASA Goddard Space Flight Center (GSFC)
Laboratoire d'Etude du Rayonnement et de la Matière en Astrophysique (LERMA (UMR_8112))
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris
Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-CY Cergy Paris Université (CY)
Source :
Earth System Science Data, Earth System Science Data, Copernicus Publications, 2021, 13 (5), pp.2001-2023. ⟨10.5194/essd-13-2001-2021⟩, Earth System Science Data, Vol 13, Pp 2001-2023 (2021)
Publication Year :
2021
Publisher :
HAL CCSD, 2021.

Abstract

Seasonal and interannual variations in global wetland area are a strong driver of fluctuations in global methane (CH4) emissions. Current maps of global wetland extent vary in their wetland definition, causing substantial disagreement between and large uncertainty in estimates of wetland methane emissions. To reconcile these differences for large-scale wetland CH4 modeling, we developed the global Wetland Area and Dynamics for Methane Modeling (WAD2M) version 1.0 dataset at a ∼ 25 km resolution at the Equator (0.25∘) at a monthly time step for 2000–2018. WAD2M combines a time series of surface inundation based on active and passive microwave remote sensing at a coarse resolution with six static datasets that discriminate inland waters, agriculture, shoreline, and non-inundated wetlands. We excluded all permanent water bodies (e.g., lakes, ponds, rivers, and reservoirs), coastal wetlands (e.g., mangroves and sea grasses), and rice paddies to only represent spatiotemporal patterns of inundated and non-inundated vegetated wetlands. Globally, WAD2M estimates the long-term maximum wetland area at 13.0×106 km2 (13.0 Mkm2), which can be divided into three categories: mean annual minimum of inundated and non-inundated wetlands at 3.5 Mkm2, seasonally inundated wetlands at 4.0 Mkm2 (mean annual maximum minus mean annual minimum), and intermittently inundated wetlands at 5.5 Mkm2 (long-term maximum minus mean annual maximum). WAD2M shows good spatial agreements with independent wetland inventories for major wetland complexes, i.e., the Amazon Basin lowlands and West Siberian lowlands, with Cohen's kappa coefficient of 0.54 and 0.70 respectively among multiple wetland products. By evaluating the temporal variation in WAD2M against modeled prognostic inundation (i.e., TOPMODEL) and satellite observations of inundation and soil moisture, we show that it adequately represents interannual variation as well as the effect of El Niño–Southern Oscillation on global wetland extent. This wetland extent dataset will improve estimates of wetland CH4 fluxes for global-scale land surface modeling. The dataset can be found at https://doi.org/10.5281/zenodo.3998454 (Zhang et al., 2020).

Details

Language :
English
ISSN :
18663508
Database :
OpenAIRE
Journal :
Earth System Science Data, Earth System Science Data, Copernicus Publications, 2021, 13 (5), pp.2001-2023. ⟨10.5194/essd-13-2001-2021⟩, Earth System Science Data, Vol 13, Pp 2001-2023 (2021)
Accession number :
edsair.doi.dedup.....a4320a68d62776c7500aa737c912872f
Full Text :
https://doi.org/10.5194/essd-13-2001-2021⟩