Citation: | Zhen-quan Lu, Chu-guo Wu, Neng-you Wu, Hai-long Lu, Ting Wang, Rui Xiao, Hui Liu, Xin-he Wu, 2022. Change trend of natural gas hydrates in permafrost on the Qinghai-Tibet Plateau (1960‒2050) under the background of global warming and their impacts on carbon emissions, China Geology, 5, 475-509. doi: 10.31035/cg2022034 |
Global warming and the response to it have become a topic of concern in today’s society and are also a research focus in the global scientific community. As the world’s third pole, the global warming amplifier, and the starting region of China’s climate change, the Qinghai-Tibet Plateau is extremely sensitive to climate change. The permafrost on the Qinghai-Tibet Plateau is rich in natural gas hydrates (NGHs) resources. Under the background of global warming, whether the NGHs will be disassociated and enter the atmosphere as the air temperature rises has become a major concern of both the public and the scientific community. Given this, this study reviewed the trend of global warming and accordingly summarized the characteristics of the temperature increase in the Qinghai-Tibet Plateau. Based on this as well as the distribution characteristics of the NGHs in the permafrost on the Qinghai-Tibet Plateau, this study investigated the changes in the response of the NGHs to global warming, aiming to clarify the impacts of global warming on the NGHs in the permafrost of the plateau. A noticeable response to global warming has been observed in the Qinghai-Tibet Plateau. Over the past decades, the increase in the mean annual air temperature of the plateau was increasingly high and more recently. Specifically, the mean annual air temperature of the plateau changed at a rate of approximately 0.308‒0.420°C/10a and increased by approximately 1.54‒2.10°C in the past decades. Moreover, the annual mean ground temperature of the shallow permafrost on the plateau increased by approximately 1.155‒1.575°C and the permafrost area decreased by approximately 0.34×106 km2 from about 1.4×106 km2 to 1.06×106 km2 in the past decades. As indicated by simulated calculation results, the thickness of the NGH-bearing permafrost on the Qinghai-Tibet Plateau has decreased by 29‒39 m in the past 50 years, with the equivalent of (1.69‒2.27)×1010‒(1.12‒1.51)×1012 m3 of methane (CH4) being released due to NGHs dissociation. It is predicted that the thickness of the NGH-bearing permafrost will decrease by 23 m and 27 m, and dissociated and released NGHs will be the equivalent of (1.34‒88.8)×1010 m3 and (1.57‒104)×1010 m3 of CH4, respectively by 2030 and 2050. Considering the positive feedback mechanism of NGHs on global warming and the fact that CH4 has a higher greenhouse effect than carbon dioxide, the NGHs in the permafrost on the Qinghai-Tibet Plateau will emit more CH4 into the atmosphere, which is an important trend of NGHs under the background of global warming. Therefore, the NGHs are destructive as a time bomb and may lead to a waste of efforts that mankind has made in carbon emission reduction and carbon neutrality. Accordingly, this study suggests that human beings should make more efforts to conduct the exploration and exploitation of the NGHs in the permafrost of the Qinghai-Tibet Plateau, accelerate research on the techniques and equipment for NGHs extraction, storage, and transportation, and exploit the permafrost-associated NGHs while thawing them. The purpose is to reduce carbon emissions into the atmosphere and mitigate the atmospheric greenhouse effect, thus contributing to the global goal of peak carbon dioxide emissions and carbon neutrality.
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Global distribution of permafrost areas (after Zhao SM et al., 2022).
Curves of atmospheric CO2 and CH4 concentrations reconstructed from Antarctic ice cores and synthetic temperature curve (after Beeman JC et al., 2019).
Sketch map showing the distribution of the permafrost on the Qinghai-Tibet Plateau (modified from Zhou YW et al., 2000).
Global mean temperature anomalies in the past 2000 years reconstructed based on proxy data (after PAGES 2K Consortium et al., 2019).
Paleoclimate records of the Kunlun Pass (KP) section of northern Qinghai-Tibet Plateau and global proxies (after Cheng F et al., 2022).
Correlation between the warming trends of the Qinghai-Tibet Plateau and the Northern Hemisphere (after Yao TD et al., 2006).
Thickness of active layer in permafrost area along Qinghai-Tibet Highway and the temperature change at the bottom of the active layer (after National Climate Change Centre, China Meteorological Administration, 2022).
Characteristics of the mean temperature before and after the abrupt change of the Qinghai-Tibet Plateau from 1961 to 2010 (Xu LJ et al., 2019).
Map showing the distribution of NGH prospect areas in China (modified from Zhu YH et al., 2011).
Map showing the distribution of drilled wells that encountered natural gas hydrates and the location of a production test in the Qilian Mountains permafrost region in the Qinghai-Tibet Plateau (after Lu ZQ et al., 2020).
Natural gas hydrates collected from wells drilled in the Qinghai-Tibet Plateau (after Lu ZQ et al., 2011).
Histograms showing the horizons of the natural gas hydrates and permafrost in the Qilian Mountains permafrost region on the Qinghai-Tibet Plateau (after Lu ZQ et al., 2020).
Gas hydrate genetic diagrams of C1/(C2+C3) vs. δ13C1 (left) and δDC1 vs. δ13C1 (right) (after Lu Z et al., 2011).
Effects of permafrost changes on the NGHs of the Qinghai-Tibet Plateau under the background of global warming (modified from Wang PK et al., 2014).
Changes in NGHs formation conditions under different permafrost thicknesses (left) and the influence of temperature and pressure on NGHs (right) (after Lu ZQ et al., 2008).
Prediction of the air temperature, reduced thickness of hydrates and released CH4 on the Qinghai-Tibet Plateau in the next 30 years.