13 June 2024

Climate change and plant growth on the Tibetan Plateau

Climate change

The ratio between above- and below-ground growth is shown here. For most polar plant species, the below-ground parts are larger than above-ground parts. The question is how the ratio has changed and will change in the future due to changes in climate.

The Tibetan Plateau
The Tibetan Plateau, also known as the "Roof of the World" is the highest and largest plateau above sea level located in Central, South, and East Asia. The area stretches about 1,000 km north to south and 2,500 km east to west. It is a vast area of 2,500,000 km2 with wide-spread permafrost due to an average elevation of 4,500 m. Currently, changes in climate includes warming but also increasing lack of water during the growing season. Hanbo Yun

Global warming over the last three decades has significantly altered patterns of plant growth on the Tibetan Plateau. Plants have been shown to adjust their growth trajectories in response to climate change. For example, by prioritizing growth of leaves and stems or the extension of their roots, plants can better capture nutrients from the Sun and atmosphere or the soil. These dynamics are particularly important to understand in permafrost regions, where substantial amounts of carbon dioxide are absorbed, stored, and emitted. However, the relationship between changes in above- relative to below-ground growth is not well understood.

The ratio between above- and below-ground growth is shown here. For most polar plant species, the below-ground parts are larger than above-ground parts. The question is how the ratio has changed and will change in the future due to changes in climate. Yanpeng Zhu

A new international study including colleagues from Key Laboratory of Cryospheric Science and Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences in Lanzhou (in Gansu, China) and Department of Geosciences and Natural Resource Management at University of Copenhagen, have collected and analyzed plant samples and meteorological data from eight sites across the continuous permafrost region of the Tibetan Plateau between 1995 and 2021. Results of the study show that plants in the alpine wetlands had more aboveground growth (a marked increase of 17%), while plants in the drier alpine meadows and steppes had more belowground growth (a decrease of 26% and 48%, respectively).

First-author and PhD student Hanbo Yun explains, that these trends were driven primarily by changes in soil temperature, an effect that increased three-fold over the study period. In the meadows and steppes, where water is more scarce than the wetlands, greater moisture in the soil made the plants more sensitive to temperature changes. Current ecosystem models were not able to reproduce these vegetation type specific observations. According to the authors, these results may be used to improve projections of carbon cycling in permafrost ecosystems.

LINK: Article #2023-14036:

https://doi.org/10.1073/pnas.2314036121

Further information please contact

Hanbo Yun, PhD student
Department of Geosciences and Natural Resource Management
University of Copenhagen
hanbo.yun@ign.ku.dk


Bo Elberling, professor
Department of Geosciences and Natural Resource Management
University of Copenhagen
+45 23 63 84 53
be@ign.ku.dk

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