---
res:
  bibo_abstract:
  - High elevation headwater catchments are complex hydrological systems that seasonally
    buffer water and release it in the form of snow and ice melt, modulating downstream
    runoff regimes and water availability. In High Mountain Asia (HMA), where a wide
    range of climates from semi-arid to monsoonal exist, the importance of the cryospheric
    contributions to the water budget varies with the amount and seasonal distribution
    of precipitation. Losses due to evapotranspiration and sublimation are to date
    largely unquantified components of the water budget in such catchments, although
    they can be comparable in magnitude to glacier melt contributions to streamflow.
    Here, we simulate the hydrology of three high elevation headwater catchments in
    distinct climates in HMA over 10 years using an ecohydrological model geared towards
    high-mountain areas including snow and glaciers, forced with reanalysis data.
    Our results show that evapotranspiration and sublimation together are most important
    at the semi-arid site, Kyzylsu, on the northernmost slopes of the Pamir mountain
    range. Here, the evaporative loss amounts to 28% of the water throughput, which
    we define as the total water added to, or removed from the water balance within
    a year. In comparison, evaporative losses are 19% at the Central Himalayan site
    Langtang and 13% at the wettest site, 24 K, on the Southeastern Tibetan Plateau.
    At the three sites, respectively, sublimation removes 15%, 13% and 6% of snowfall,
    while evapotranspiration removes the equivalent of 76%, 28% and 19% of rainfall.
    In absolute terms, and across a comparable elevation range, the highest ET flux
    is 413 mm yr−1 at 24 K, while the highest sublimation flux is 91 mm yr−1 at Kyzylsu.
    During warm and dry years, glacier melt was found to only partially compensate
    for the annual supply deficit.@eng
  bibo_authorlist:
  - foaf_Person:
      foaf_givenName: S
      foaf_name: Fugger, S
      foaf_surname: Fugger
  - foaf_Person:
      foaf_givenName: T E
      foaf_name: Shaw, T E
      foaf_surname: Shaw
  - foaf_Person:
      foaf_givenName: A
      foaf_name: Jouberton, A
      foaf_surname: Jouberton
  - foaf_Person:
      foaf_givenName: E S
      foaf_name: Miles, E S
      foaf_surname: Miles
  - foaf_Person:
      foaf_givenName: P
      foaf_name: Buri, P
      foaf_surname: Buri
  - foaf_Person:
      foaf_givenName: M
      foaf_name: McCarthy, M
      foaf_surname: McCarthy
  - foaf_Person:
      foaf_givenName: C
      foaf_name: Fyffe, C
      foaf_surname: Fyffe
  - 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: M
      foaf_name: Kneib, M
      foaf_surname: Kneib
  - foaf_Person:
      foaf_givenName: Peter
      foaf_name: Molnar, Peter
      foaf_surname: Molnar
  - foaf_Person:
      foaf_givenName: F
      foaf_name: Pellicciotti, F
      foaf_surname: Pellicciotti
  bibo_doi: 10.1088/1748-9326/ad25a0
  bibo_issue: '4'
  bibo_volume: 19
  dct_date: 2024^xs_gYear
  dct_isPartOf:
  - http://id.crossref.org/issn/1748-9326
  dct_language: eng
  dct_publisher: IOP Publishing@
  dct_subject:
  - Glacio-hydrology
  - High mountain Asia
  - High mountain hydrology
  - Ecohydrology
  - Landsurface modelling
  - Remote sensing hydrology
  dct_title: Hydrological regimes and evaporative flux partitioning at the climatic
    ends of high mountain Asia@
...