---
res:
  bibo_abstract:
  - Glacier health across High Mountain Asia (HMA) is highly heterogeneous and strongly
    governed by regional climate, which is variably influenced by monsoon dynamics
    and the westerlies. We explore four decades of glacier energy and mass balance
    at three climatically distinct sites across HMA by utilising a detailed land surface
    model driven by bias-corrected Weather Research and Forecasting meteorological
    forcing. All three glaciers have experienced long-term mass losses (ranging from
    −0.04 ± 0.09 to −0.59 ± 0.20 m w.e. a−1) consistent with widespread warming across
    the region. However, complex and contrasting responses of glacier energy and mass
    balance to the patterns of the Indian Summer Monsoon were evident, largely driven
    by the role snowfall timing, amount and phase. A later monsoon onset generates
    less total snowfall to the glacier in the southeastern Tibetan Plateau during
    May–June, augmenting net shortwave radiation and affecting annual mass balance
    (−0.5 m w.e. on average compared to early onset years). Conversely, timing of
    the monsoon’s arrival has limited impact for the Nepalese Himalaya which is more
    strongly governed by the temperature and snowfall amount during the core monsoon
    season. In the arid central Tibetan Plateau, a later monsoon arrival results in
    a 40 mm (58%) increase of May–June snowfall on average compared to early onset
    years, likely driven by the greater interaction of westerly storm events. Meanwhile,
    a late monsoon cessation at this site sees an average 200 mm (192%) increase in
    late summer precipitation due to monsoonal storms. A trend towards weaker intensity
    monsoon conditions in recent decades, combined with long-term warming patterns,
    has produced predominantly negative glacier mass balances for all sites (up to
    1 m w.e. more mass loss in the Nepalese Himalaya compared to strong monsoon intensity
    years) but sub-regional variability in monsoon timing can additionally complicate
    this response.@eng
  bibo_authorlist:
  - foaf_Person:
      foaf_givenName: T E
      foaf_name: Shaw, T E
      foaf_surname: Shaw
  - foaf_Person:
      foaf_givenName: E S
      foaf_name: Miles, E S
      foaf_surname: Miles
  - foaf_Person:
      foaf_givenName: D
      foaf_name: Chen, D
      foaf_surname: Chen
  - foaf_Person:
      foaf_givenName: A
      foaf_name: Jouberton, A
      foaf_surname: Jouberton
  - foaf_Person:
      foaf_givenName: M
      foaf_name: Kneib, M
      foaf_surname: Kneib
  - foaf_Person:
      foaf_givenName: S
      foaf_name: Fugger, S
      foaf_surname: Fugger
  - foaf_Person:
      foaf_givenName: T
      foaf_name: Ou, T
      foaf_surname: Ou
  - foaf_Person:
      foaf_givenName: H-W
      foaf_name: Lai, H-W
      foaf_surname: Lai
  - foaf_Person:
      foaf_givenName: K
      foaf_name: Fujita, K
      foaf_surname: Fujita
  - foaf_Person:
      foaf_givenName: W
      foaf_name: Yang, W
      foaf_surname: Yang
  - foaf_Person:
      foaf_givenName: Simone
      foaf_name: Fatichi, Simone
      foaf_surname: Fatichi
      foaf_workInfoHomepage: http://www.librecat.org/personId=cf8e546b-a9b0-11f0-a43b-aa89ed1b56d6
  - foaf_Person:
      foaf_givenName: F
      foaf_name: Pellicciotti, F
      foaf_surname: Pellicciotti
  bibo_doi: 10.1088/1748-9326/ac9008
  bibo_issue: '10'
  bibo_volume: 17
  dct_date: 2022^xs_gYear
  dct_isPartOf:
  - http://id.crossref.org/issn/1748-9326
  dct_language: eng
  dct_publisher: IOP Publishing@
  dct_subject:
  - Glacier
  - Long-term mass balance
  - Monsoon
  - Snowfall
  dct_title: Multi-decadal monsoon characteristics and glacier response in High Mountain
    Asia@
...