###### Abstract  
The Three Rivers Source Region (TRSR) is a natural habitat for rare animals and a genetic treasure trove of plateau organisms. It is an important eco-safety barrier in China and even Asia, and a priority of China's to promote ecological advancement. Precisely assessing the dynamics and mechanisms of alpine grassland ecosystem carbon budgets is beneficial for quantifying the response to climate change on a regional scale. The spatial distribution and dynamic changes in carbon fluxes in the TRSR from 1985 to 2018 were analyzed by the Theil-Sen + Mann-Kendall and ensemble empirical mode decomposition (EEMD) methods, and multiple linear regression was used to quantify the contribution of meteorological elements to the carbon flux trends. The results indicated that (1) the alpine grassland ecosystem was a weak carbon sink. The multiyear mean gross primary production (GPP) and net ecosystem production (NEP) in the TRSR were 147.86 and 11.27 g C/m\({}^{2}\)/yr, respectively. The distribution of carbon fluxes progressively decreased from east to west. (2) The carbon fluxes of the alpine grassland ecosystem were dominated by a monotonically increasing trend, with increasing rates of GPP and NEP of 1.31 and 0.40 g C/m\({}^{2}\)/yr, respectively. A total of 48.60% of the alpine grassland showed a significant increase in NEP, whereas only 0.21% showed a significant decrease during the research term. (3) The alpine meadow sequestered carbon better than the alpine stepping did and accounted for more than 60% of the regional carbon sink. (4) In a correlation analysis between NEP and temperature, precipitation and solar radiation, the positive correlation accounted for 89.67%, 90.51%, and 21.16% of the TRSR, respectively. Rising temperatures and increased precipitation were the main drivers contributing to the increase in NEP. Research on carbon budget variability and mechanisms can help guide preservation zoning initiatives in national parks. alpine grassland; net ecosystem productivity; three rivers source region; EEMD Article  
The Three Rivers Source Region Alpine Grassland Ecosystem Was a Weak Carbon Sink Based on BEPS Model Analysis  
[PERSON]  
1  
in recent decades. For example, the rate of annual average temperature increase over the past half century has been 0.4 \({}^{\circ}\)C/10 years [13], which is more than double the rate of the global temperature rise [14], and the region is likely to continue to warm this century [15]. Precipitation in the winter and spring, on the other hand, has increased substantially, whereas precipitation in other seasons has not noticeably varied [16; 17]. In addition, it is worth noting that the TRSR is experiencing vegetation deterioration, glacier retreat, wetland depletion, and decreased species diversity [18; 19; 20]. To halt the degradation of the ecological environment of the TRSR, the administration launched ecological protection and restoration of TRSR reserve zones in 2005. The government initiated the \"Pilot Program of Three Rivers Source Region National Park System\" in 2015, and the Three Rivers Source National Park (TRSNP) was codified in 2018 and proclaimed in 2021 [21]. Consequently, regional vegetation changes should be analyzed under the combined effect of climate change and human policy. The balance between gross primary production (GPP) and ecosystem respiration (ER) is described as net ecosystem production (NEP), which is a crucial measure of ecosystem carbon budgets [22]. Due to the special geographical environment of the TRSR, such as its higher solar radiation and cooler temperature, the carbon budget of this ecosystem is of particular concern [23], but carbon source/sink dynamics are extremely unpredictable [24; 25; 26]. According to certain investigations, alpine meadows serve as \"carbon sinks\" [22; 27; 28; 29; 30].