---
_id: '12577'
abstract:
- lang: eng
  text: Glaciers are key components of the mountain water towers of Asia and are vital
    for downstream domestic, agricultural, and industrial uses. The glacier mass loss
    rate over the southeastern Tibetan Plateau is among the highest in Asia and has
    accelerated in recent decades. This acceleration has been attributed to increased
    warming, but the mechanisms behind these glaciers’ high sensitivity to warming
    remain unclear, while the influence of changes in precipitation over the past
    decades is poorly quantified. Here, we reconstruct glacier mass changes and catchment
    runoff since 1975 at a benchmark glacier, Parlung No. 4, to shed light on the
    drivers of recent mass losses for the monsoonal, spring-accumulation glaciers
    of the Tibetan Plateau. Our modeling demonstrates how a temperature increase (mean
    of 0.39<jats:sup>∘</jats:sup>C ⋅dec<jats:sup>−1</jats:sup>since 1990) has accelerated
    mass loss rates by altering both the ablation and accumulation regimes in a complex
    manner. The majority of the post-2000 mass loss occurred during the monsoon months,
    caused by simultaneous decreases in the solid precipitation ratio (from 0.70 to
    0.56) and precipitation amount (–10%), leading to reduced monsoon accumulation
    (–26%). Higher solid precipitation in spring (+18%) during the last two decades
    was increasingly important in mitigating glacier mass loss by providing mass to
    the glacier and protecting it from melting in the early monsoon. With bare ice
    exposed to warmer temperatures for longer periods, icemelt and catchment discharge
    have unsustainably intensified since the start of the 21st century, raising concerns
    for long-term water supply and hazard occurrence in the region.
article_number: e2109796119
article_processing_charge: No
article_type: original
author:
- first_name: Achille
  full_name: Jouberton, Achille
  last_name: Jouberton
- first_name: Thomas E.
  full_name: Shaw, Thomas E.
  last_name: Shaw
- first_name: Evan
  full_name: Miles, Evan
  last_name: Miles
- first_name: Michael
  full_name: McCarthy, Michael
  last_name: McCarthy
- first_name: Stefan
  full_name: Fugger, Stefan
  last_name: Fugger
- first_name: Shaoting
  full_name: Ren, Shaoting
  last_name: Ren
- first_name: Amaury
  full_name: Dehecq, Amaury
  last_name: Dehecq
- first_name: Wei
  full_name: Yang, Wei
  last_name: Yang
- first_name: Francesca
  full_name: Pellicciotti, Francesca
  id: b28f055a-81ea-11ed-b70c-a9fe7f7b0e70
  last_name: Pellicciotti
citation:
  ama: Jouberton A, Shaw TE, Miles E, et al. Warming-induced monsoon precipitation
    phase change intensifies glacier mass loss in the southeastern Tibetan Plateau.
    <i>PNAS</i>. 2022;119(37). doi:<a href="https://doi.org/10.1073/pnas.2109796119">10.1073/pnas.2109796119</a>
  apa: Jouberton, A., Shaw, T. E., Miles, E., McCarthy, M., Fugger, S., Ren, S., …
    Pellicciotti, F. (2022). Warming-induced monsoon precipitation phase change intensifies
    glacier mass loss in the southeastern Tibetan Plateau. <i>PNAS</i>. Proceedings
    of the National Academy of Sciences. <a href="https://doi.org/10.1073/pnas.2109796119">https://doi.org/10.1073/pnas.2109796119</a>
  chicago: Jouberton, Achille, Thomas E. Shaw, Evan Miles, Michael McCarthy, Stefan
    Fugger, Shaoting Ren, Amaury Dehecq, Wei Yang, and Francesca Pellicciotti. “Warming-Induced
    Monsoon Precipitation Phase Change Intensifies Glacier Mass Loss in the Southeastern
    Tibetan Plateau.” <i>PNAS</i>. Proceedings of the National Academy of Sciences,
    2022. <a href="https://doi.org/10.1073/pnas.2109796119">https://doi.org/10.1073/pnas.2109796119</a>.
  ieee: A. Jouberton <i>et al.</i>, “Warming-induced monsoon precipitation phase change
    intensifies glacier mass loss in the southeastern Tibetan Plateau,” <i>PNAS</i>,
    vol. 119, no. 37. Proceedings of the National Academy of Sciences, 2022.
  ista: Jouberton A, Shaw TE, Miles E, McCarthy M, Fugger S, Ren S, Dehecq A, Yang
    W, Pellicciotti F. 2022. Warming-induced monsoon precipitation phase change intensifies
    glacier mass loss in the southeastern Tibetan Plateau. PNAS. 119(37), e2109796119.
  mla: Jouberton, Achille, et al. “Warming-Induced Monsoon Precipitation Phase Change
    Intensifies Glacier Mass Loss in the Southeastern Tibetan Plateau.” <i>PNAS</i>,
    vol. 119, no. 37, e2109796119, Proceedings of the National Academy of Sciences,
    2022, doi:<a href="https://doi.org/10.1073/pnas.2109796119">10.1073/pnas.2109796119</a>.
  short: A. Jouberton, T.E. Shaw, E. Miles, M. McCarthy, S. Fugger, S. Ren, A. Dehecq,
    W. Yang, F. Pellicciotti, PNAS 119 (2022).
date_created: 2023-02-20T08:10:02Z
date_published: 2022-09-06T00:00:00Z
date_updated: 2023-02-28T13:50:37Z
day: '06'
doi: 10.1073/pnas.2109796119
extern: '1'
intvolume: '       119'
issue: '37'
keyword:
- Multidisciplinary
language:
- iso: eng
month: '09'
oa_version: None
publication: PNAS
publication_identifier:
  eissn:
  - 1091-6490
  issn:
  - 0027-8424
publication_status: published
publisher: Proceedings of the National Academy of Sciences
quality_controlled: '1'
scopus_import: '1'
status: public
title: Warming-induced monsoon precipitation phase change intensifies glacier mass
  loss in the southeastern Tibetan Plateau
type: journal_article
user_id: 2DF688A6-F248-11E8-B48F-1D18A9856A87
volume: 119
year: '2022'
...
