Spatiotemporal Evolution and Driving Mechanism of NEP in Qilian Mountain National Park

Authors

  • Jinfei Jiao

DOI:

https://doi.org/10.62051/ijnres.v8n4.05

Keywords:

Qilian Mountain National Park; Carbon Sink; Carbon Source; Spatiotemporal Variation; Net Ecosystem Productivity.

Abstract

Taking Qilian Mountain National Park as the study area, this research systematically analyzed the spatiotemporal evolution characteristics and driving mechanisms of carbon sources/sinks in the park based on the MOD17A3HGF net primary productivity (NPP) dataset and meteorological data including temperature, precipitation, humidity, and sunshine duration from 2000 to 2022. The methods applied included a net ecosystem productivity (NEP) estimation model, pixel-wise linear regression, and correlation analysis. The results showed that: From 2000 to 2022, the park’s NEP exhibited a fluctuating upward trend with a slope of 1.89 gCm2a, reaching a peak of 181.6 gCm2a in 2019. The region was dominated by carbon sinks overall, with carbon source areas accounting for less than 0.5% and showing a decreasing trend. Spatially, NEP was higher in the southeast and lower in the northwest. High-value areas were concentrated in the Eastern Qilian Mountains spruce forest–alpine meadow and Hexi Corridor arid desert–oasis agricultural ecological subzones, while low-value areas were distributed in the Qaidam Basin desert, Western Qilian Mountains alpine desert steppe, and Qinghai Lake Wetland alpine meadow subzone. NEP showed an increasing trend across all five ecological subzones, with growth rates ranked as: Hexi Corridor (3.88) > Eastern Qilian Mountains (2.31) > Western Qilian Mountains (1.3) > Qaidam Basin (1.02) > Qinghai Lake Wetland (0.25). An increasing NEP trend occurred in 98.8% of the park area, among which 73.4% showed an extremely significant increase. NEP was positively correlated with meteorological factors; temperature was the primary driving factor, followed by precipitation and humidity, while sunshine duration had a relatively weak effect. This study can provide a scientific basis for ecological conservation, restoration, and carbon sink enhancement in Qilian Mountain National Park.

References

[1] Yu L, Pu S L. New understanding of the IPCC Fifth Assessment Report on carbon cycle and other biogeochemical cycles[J]. Progressus Inquisitiones de Mutatione Climatis, 2014, 10(1): 33-36.

[2] Qian Z, Bathiany S, Liu T, et al. Decadal sink-source shifts of forest aboveground carbon since 1988[J]. arXiv preprint arXiv:2506.11879, 2025.

[3] Hou Q, Yu X. Seasonal variation in carbon flux and the driving mechanisms in the grassland ecosystem in a mountain region of Northwest China[J]. Ecological Indicators, 2025, 179: 114168.

[4] Liu X X, Hao Y Y, Meng Z, et al. Spatiotemporal changes and driving factors of carbon storage in Qilian Mountain National Park from 1990 to 2022[J]. Acta Ecologica Sinica, 2025, 45(11): 5263-5276.

[5] Zhao F Y, Wang Q F, Zhang H T, et al. Spatiotemporal variation of arbor forest carbon storage in Qilian Mountain forest region of Gansu Province based on the InVEST model[J]. Journal of Northwest Forestry University, 2023, 38(4): 233–240.

[6] Hou Q Q. Characteristics, influencing factors and future projection of carbon budget changes in grassland ecosystems of the Qilian Mountains [D]. Gansu Agricultural University, 2025.

[7] Li N, Li Q S, Li H T. Study on carbon storage and carbon sink value of forest vegetation in the Qinghai Section of Qilian Mountain National Park[J]. Journal of Zhejiang Forestry Science and Technology, 2021, 41(2): 41–46.

[8] Raich J W, Rastetter E B, Melillo J M, et al. Potential net primary productivity in South America: application of a global model[J]. Ecological applications, 1991, 1(4): 399-429.

[9] Ming-Kui C A O, Bo T, Ke-Rang L I, et al. Interannual variation in terrestrial ecosystem carbon fluxes in China from 1981 to 1998[J]. Journal of Integrative Plant Biology, 2003, 45(5): 552.

[10] Luyssaert S, Schulze E D, Börner A, et al. Old-growth forests as global carbon sinks[J]. Nature, 2008, 455(7210): 213-215.

[11] Fang J Y, Guo Z D, Pu S L, et al. Estimation of carbon sinks in terrestrial vegetation in China from 1981 to 2000[J]. Science in China Series D: Earth Sciences, 2007, (6): 804–812.

[12] Pei Z Y, Zhou C P, Ouyang H, et al. Carbon estimation in alpine steppe regions of the Qinghai-Tibet Plateau [J]. Geographical Research, 2010, 29(1): 102–110.

[13] Li D K, Fan J Z, Wang J. Variation characteristics of vegetation NPP in Shaanxi Province based on MOD17A3 [J]. Chinese Journal of Ecology, 2011, 30(12): 2776–2782.

[14] Song Y, Ma M G. Analysis of vegetation cover changes in Northwest China based on SPOT VEGETATION data [J]. Journal of Desert Research, 2007, (1): 89–93+ 173.

[15] Liu J Q, Li J J, Di H. Estimation of net primary production, carbon storage and carbon sink function of forest vegetation in Qilian Mountains [J]. Journal of Northwest Forestry University, 2017, 32(2): 1–7+42.

[16] Tang Z H, Wei Q S, Liu H J, et al. Characteristics of alpine vegetation communities and their relationships with topographic and climatic factors in the eastern Qilian Mountains [J]. Acta Ecologica Sinica, 2020, 40(1): 223–232.

[17] Sun R B, Lu Q Z, Ma S H. Ecological status and degradation causes of Qilian Mountain region in Qinghai [J]. Qinghai Prataculture, 2009, 18(3): 19–26+18.

[18] Liu F, Zeng Y N. Spatiotemporal patterns and changes of vegetation carbon source/sink in the Qinghai Plateau from 2000 to 2015 [J]. Acta Ecologica Sinica, 2021, 41(14): 5792–5803.

[19] Chen G C, Peng M, Huang R F, et al. Vegetation characteristics and distribution patterns in the Qilian Mountains region [J]. Acta Botanica Sinica, 1994, (1): 63–72.

[20] Niu H H, Chen H, Fu Y, et al. Niche characteristics of desert plants in the eastern Qaidam Basin [J]. Acta Ecologica Sinica, 2019, 39(8): 2862–2871.

[21] Tang Z H, Wei Q S, Liu H J, et al. Characteristics of alpine vegetation communities and their relationships with topographic and climatic factors in the eastern Qilian Mountains [J]. Acta Ecologica Sinica, 2020, 40(1): 223–232.

[22] Jia J H, Liu H Y, Lin Z S. Multi-temporal scale changes of vegetation NPP and its response to climate change in Northwest China [J]. Acta Ecologica Sinica, 2019, 39(14): 5058–5069.

[23] Shang S S, Lian L S, Ma T, et al. Spatiotemporal variation characteristics of air temperature and precipitation in Northwest China in recent 54 years [J]. Arid Zone Research, 2018, 35(1): 68–76.

[24] Zhang Z Q, Cai H W, Zhang P P, et al. Spatiotemporal changes of vegetation carbon source/sink in the Three-River Headwaters Region based on GEE remote sensing cloud platform [J]. Remote Sensing for Natural Resources, 2023, 35(1): 231–242.

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Published

30-04-2026

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Articles

How to Cite

Jiao, J. (2026). Spatiotemporal Evolution and Driving Mechanism of NEP in Qilian Mountain National Park. International Journal of Natural Resources and Environmental Studies, 8(4), 41-52. https://doi.org/10.62051/ijnres.v8n4.05