by Zhang Nannan, Chinese Academy of Sciences

The process of soil wind erosion is influenced by vegetation cover. From a functional point of view, vegetation can be divided into photosynthetic vegetation (PV) and non-photosynthetic vegetation (NPV). The NPV represents dormant and dead vegetation, crop residues, and litter, which are the main components of surface vegetation during the non-growing season. It also helps to reduce wind erosion during this time. However, the normalized difference vegetation index (NDVI) can generally reflect the fractional cover of PV, but it may not accurately reflect the fractional cover of NPV, leading to potential errors in estimating the fractional cover of NPV.

1 s2.0 S0016706124001095 gr1 lrg cas res
Map of the Mu Us Sandy Land and distributions of field investigation sites: a. location, land use types (2020), field spectral sites and observation sites in the Mu Us Sandy Land, b. Big Spring Number Eight sand collector, c. ultrasonic anemometer (surrounded by a red oval) c. process of collecting spectra in the Mu Us Sandy Land. Credit: Geoderma (2024). DOI: 10.1016/j.geoderma.2024.116880

A research team from the Northwest Institute of Eco-Environment and Resources of the Chinese Academy of Sciences collected hyperspectral data on NPV to estimate the fractional coverage in the Mu Us Sandy Land (MUSL) using Landsat 8-OLI images from 2014 to 2017.

In the study published in Geoderma, the researchers conducted short-term observations of wind erosion to estimate the fractional cover of NPV and calibrate the simulated results to reduce uncertainties in wind erosion simulations.

They found that the mean values of NPV fractional cover in the MUSL from 2014 to 2017 were approximately 2.71 times higher than those estimated from NDVI data.

After coupling NPV into the revised wind erosion equation model, the simulation accuracy of this model obviously increased, which was validated by observational data.

Without considering NPV, the wind erosion modulus is overestimated. The wind erosion modulus was overestimated at rates of 130.48 t/km2/a, 91.79 t/km2/a, 85.51 t/km2/a, and 93.76 t/km2/a from 2014 to 2017, respectively. The corresponding wind erosion overestimation rates for these years were 26.52%, 16.9%, 21.47% and 31.33%, respectively.

In this study, NPV was integrated into the RWEQ model to enhance the simulation accuracy of this model and to provide a new perspective for the future development of wind erosion models.

This article is republished under a Creative Commons Attribution 4.0 International License. Read the original article.

(More information: Xiufan Liu et al, ‘An improvement of the Revised Wind Erosion Equation by considering the effect of non-photosynthetic vegetation’, Geoderma (2024). DOI: 10.1016/j.geoderma.2024.116880)

Small iceberg floating in ocean water under a bright sky with the Sun visible above - climate change effects (s. science, climate, Muser)
Climate Science Digest: March 12, 2025Science

Climate Science Digest: March 12, 2025

Explore the latest insights from top science journals in the Muser Press daily roundup, featuring impactful research on climate change challenges. In brief: In the…
Muser NewsDeskMuser NewsDeskMarch 12, 2025 Full article
Image: Close-up of Wheat
Making crops heat-resilient is possible, but costly and time-consumingScience

Making crops heat-resilient is possible, but costly and time-consuming

New review in Science outlines proven strategies to protect crop productivity from rising temperatures, but warns that scaling them up will take decades and major…
SourceSourceJune 19, 2025 Full article
Image: El Niño, Earth
El Niño oscillations were stronger and more frequent in Earth’s ancient pastScience

El Niño oscillations were stronger and more frequent in Earth’s ancient past

A recent study from Duke University researchers reveals that the El Niño phenomenon, a warm ocean event with global climatic impact, has been occurring for…
Adrian AlexandreAdrian AlexandreOctober 22, 2024 Full article