4.7 Article

Net Primary Productivity Estimation of Terrestrial Ecosystems in China with Regard to Saturation Effects and Its Spatiotemporal Evolutionary Impact Factors

Journal

REMOTE SENSING
Volume 15, Issue 11, Pages -

Publisher

MDPI
DOI: 10.3390/rs15112871

Keywords

net primary productivity; kernel vegetation index; spatiotemporal variation; driving mechanism

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This research utilizes a new vegetation index based on radial basis function (RBF) to estimate the net primary productivity (NPP) of Chinese terrestrial ecosystems over the past two decades (2001-2020) and investigates the spatiotemporal variation characteristics of NPP and its driving mechanisms. The kernel vegetation index (kNDVI) effectively alleviates saturation issues and improves the accuracy of NPP estimation compared to NDVI. The study finds that changes in NPP are mainly influenced by precipitation, with dominant factors varying over time and having different impacts.
The net primary productivity (NPP) of vegetation holds a pivotal character for the global carbon balance as a key parameter for characterizing terrestrial ecological processes. The most commonly used indices for estimating vegetation NPP, for instance, the normalized difference vegetation index (NDVI), often suffer from saturation issues that can compromise the accuracy of NPP estimation. This research utilizes a new vegetation index based on the radial basis function (RBF) to estimate vegetation NPP in Chinese terrestrial ecosystems over the past two decades (2001-2020) and investigates the spatiotemporal variation characteristics of NPP and the driving mechanisms. The results indicate that the kernel vegetation index (kNDVI) can effectively alleviate the saturation problem and significantly improve the accuracy of NPP estimation compared to NDVI. Over the past two decades, the NPP of Chinese terrestrial vegetation ranged from 64.13 to 79.72 g C/m(2), with a mean value of 72.75 g C/m(2), showing a fluctuating upward trend. Changes in the NPP of terrestrial ecosystems in China are mainly affected by precipitation. The dominant factors influencing NPP changes varied over time and had different impacts. For instance, in the period of 2001-2005 the climate had a positive effect on NPP changes, with the dominant factors being evaporation and precipitation. However, in the period of 2010-2015 the dominant climate factors shifted to evaporation and temperature, and their effect on NPP changes became negative. The outcomes of this research aim to serve as a foundation for carbon cycle research and ecosystem environment construction in China.

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