Abstract
<jats:p>Abstract. On 22 March 2021, an approximately 50 Mm3 ice-rock
avalanche occurred from 6500 m a.s.l. in the Sedongpu basin, southeastern
Tibet. The avalanche transformed into a highly mobile mass flow which
temporarily blocked the Yarlung Tsangpo river. The avalanche flow lasted
∼ 5 min and produced substantial geomorphological
reworking. This event, and previous ones from the basin, occurred
concurrently with, or shortly after, positive seasonal air temperature
anomalies. The occurrence of future large mass flows from the basin cannot
be ruled out, and their impacts must be carefully considered given
implications for sustainable hydropower and associated socioeconomic
development in the region.
</jats:p>
| Original language | English |
|---|---|
| Pages (from-to) | 1333-1340 |
| Number of pages | 0 |
| Journal | The Cryosphere |
| Volume | 16 |
| Issue number | 4 |
| DOIs | |
| Publication status | E-pub ahead of print - 12 Apr 2022 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 7 Affordable and Clean Energy
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Dive into the research topics of 'Brief communication: An approximately 50 Mm<sup>3</sup> ice-rock avalanche on 22 March 2021 in the Sedongpu valley, southeastern Tibetan Plateau'. Together they form a unique fingerprint.Research output
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Brief communication: A ~50 Mm<sup>3</sup> ice-rock avalanche on 22 March 2021 in the Sedongpu valley, southeastern Tibetan Plateau
Zhao, C., Yang, W., Westoby, M., An, B., Wu, G., Wang, W., Wang, Z., Wang, Y. & Dunning, S., 8 Nov 2021.Research output: Working paper / Preprint › Preprint
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