Mapping Grassland Based on Bio-Climate Probability and Intra-Annual Time-Series Abundance Data of Vegetation Habitats
-
Published:2023-09-27
Issue:19
Volume:15
Page:4723
-
ISSN:2072-4292
-
Container-title:Remote Sensing
-
language:en
-
Short-container-title:Remote Sensing
Author:
Sun Minxuan12, Ji Zhengxin1, Jiao Xin1, Lun Fei1, Sun Qiangqiang1, Sun Danfeng12ORCID
Affiliation:
1. College of Land Science and Technology, China Agricultural University, Beijing 100193, China 2. Key Laboratory of Remote Sensing for Agri-Hazards, Ministry of Agriculture, Beijing 100083, China
Abstract
Accurate inventories of grasslands are important for studies of greenhouse gas (GHG) dynamics, as grasslands store about one-third of the global terrestrial carbon stocks. This paper develops a framework for large-area grassland mapping based on the probability of grassland occurrence and the interactive pathways of fractional vegetation and soil-related endmember nexuses. In this study, grassland occurrence probability maps were produced based on data on bio-climate factors obtained from MODIS/Terra Land Surface Temperature (MOD11A2), MODIS/Terra Vegetation Indices (MOD13A3), and Tropical Rainfall Measuring Mission (TRMM 3B43) using the random forests (RF) method. Time series of 8-day fractional vegetation-related endmembers (green vegetation, non-photosynthetic vegetation, sand land, saline land, and dark surfaces) were generated using linear spectral mixture analysis (LSMA) based on MODIS/Terra Surface Reflectance data (MOD09A1). Time-series endmember fraction maps and grassland occurrence probabilities were employed to map grassland distribution using an RF model. This approach improved the accuracy by 5% compared to using endmember fractions alone. Additionally, based on the grassland occurrence probability maps, we identified extensive ecologically sensitive regions, encompassing 1.54 (104 km2) of desert-to-steppe (D-S) and 2.34 (104 km2) of steppe-to-meadow (S-M) transition regions. Among these, the D-S area is located near the threshold of 310 mm/yr in precipitation, an annual temperature of 10.16 °C, and a surface comprehensive drought index (TVPDI) of 0.59. The S-M area is situated close to the line of 437 mm/yr in precipitation, an annual temperature of 5.49 °C, and a TVPDI of 0.83.
Funder
National Natural Science Foundation of China
Subject
General Earth and Planetary Sciences
Reference51 articles.
1. Deforestation-induced climate change reduces carbon storage in remaining tropical forests;Li;Nat. Commun.,2022 2. Tiedje, J.M., Bruns, M.A., Casadevall, A., Criddle, C.S., Eloe-Fadrosh, E., Karl, D.M., Nguyen, N.K., and Zhou, J. (2022). Microbes and Climate Change: A Research Prospectus for the Future. Mbio, 13. 3. Chang, Y., Choi, D., and Kim, H. (2017). Dynamic Trends of Carbon Intensities among 127 Countries. Sustainability, 9. 4. Analysis of greenhouse gas emissions from the average Irish milk production system;Casey;Agric. Syst.,2005 5. John, W., and Nicholas, M. (2005, January 17–20). Holistic analysis of GHG emissions from Irish livestock production systems. Proceedings of the 2005 ASAE Annual Meeting, American Society of Agricultural and Biological Engineers, Tampa, FL, USA.
Cited by
1 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|