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#snowline — Public Fediverse posts

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  1. Ref 4. Contrasting patterns of change in snowline altitude across five Himalayan catchments (2025). Orie Sasak et al

    We found that long-term changes in SLA are primarily driven by shifts in the local climate, whereas seasonal variability may be influenced by geographic features in conjunction with climate.

    #research #climate #geography #snowline #altitude #LocalClimate #GlobalWarming #RiverBasin #Mountains

    🧵(5/6)

    tc.copernicus.org/articles/19/

  2. Ref 4. Contrasting patterns of change in snowline altitude across five Himalayan catchments (2025). Orie Sasak et al

    We found that long-term changes in SLA are primarily driven by shifts in the local climate, whereas seasonal variability may be influenced by geographic features in conjunction with climate.

    #research #climate #geography #snowline #altitude #LocalClimate #GlobalWarming #RiverBasin #Mountains

    🧵(5/6)

    tc.copernicus.org/articles/19/

  3. Ref 3. Cryosphere change in the warming Himalaya: Snow cover & snowline trends in Nepal’s Langtang Basin (1988-2024). D Pradhananga et al

    Snow-covered area (SCA) and its migrating lower boundary, the snowline elevation (SLE), are vital indicators of climate change and water availability in mountain regions.

    Snowline elevation rose by approximately +2.24 m/year (p = 0.088), indicating an upward shift of seasonal snowpack.
    #nepal #glaciers #snowline
    🧵(4/6)

    nepjol.info/index.php/jtha/art

  4. Ref 3. Cryosphere change in the warming Himalaya: Snow cover & snowline trends in Nepal’s Langtang Basin (1988-2024). D Pradhananga et al

    Snow-covered area (SCA) and its migrating lower boundary, the snowline elevation (SLE), are vital indicators of climate change and water availability in mountain regions.

    Snowline elevation rose by approximately +2.24 m/year (p = 0.088), indicating an upward shift of seasonal snowpack.
    #nepal #glaciers #snowline
    🧵(4/6)

    nepjol.info/index.php/jtha/art

  5. New Zealand's glaciers shrinking faster, scientist warns

    "Overall, the #snowline has been rising and in the most recent years we're seeing that rise accelerate, so we're experiencing a continued trend of glacial ice loss," said principal scientist Andrew Lorrey in a statement.

    phys.org/news/2024-03-zealand-

    #ClimateCrisis #Cryosphere #NewZealand #Glacier

  6. JWST Reveals Excess Cool Water near the #SnowLine in Compact Disks, Consistent with Pebble Drift: iopscience.iop.org/article/10. -> NASA's #Webb Findings Support Long-Proposed Process of #Planet Formation: webbtelescope.org/contents/new

  7. JWST Reveals Excess Cool Water near the #SnowLine in Compact Disks, Consistent with Pebble Drift: iopscience.iop.org/article/10. -> NASA's #Webb Findings Support Long-Proposed Process of #Planet Formation: webbtelescope.org/contents/new

  8. JWST Reveals Excess Cool Water near the #SnowLine in Compact Disks, Consistent with Pebble Drift: iopscience.iop.org/article/10. -> NASA's #Webb Findings Support Long-Proposed Process of #Planet Formation: webbtelescope.org/contents/new

  9. JWST Reveals Excess Cool Water near the #SnowLine in Compact Disks, Consistent with Pebble Drift: iopscience.iop.org/article/10. -> NASA's #Webb Findings Support Long-Proposed Process of #Planet Formation: webbtelescope.org/contents/new

  10. JWST Reveals Excess Cool Water near the #SnowLine in Compact Disks, Consistent with Pebble Drift: iopscience.iop.org/article/10. -> NASA's #Webb Findings Support Long-Proposed Process of #Planet Formation: webbtelescope.org/contents/new

  11. JWST reveals excess cool water near the #snowline in compact disks, consistent with pebble drift: arxiv.org/abs/2307.03846 -> "JWST-MIRI spectra of four disks, two compact and two large with multiple radial gaps, selected to test the scenario that water vapor inside the snowline is regulated by pebble drift. [...] These spectra clearly reveal excess emission in the low-energy lines in compact disks, compared to the large disks, establishing the presence of a cooler component with T≈ 170-400 K".

  12. JWST reveals excess cool water near the #snowline in compact disks, consistent with pebble drift: arxiv.org/abs/2307.03846 -> "JWST-MIRI spectra of four disks, two compact and two large with multiple radial gaps, selected to test the scenario that water vapor inside the snowline is regulated by pebble drift. [...] These spectra clearly reveal excess emission in the low-energy lines in compact disks, compared to the large disks, establishing the presence of a cooler component with T≈ 170-400 K".

  13. JWST reveals excess cool water near the #snowline in compact disks, consistent with pebble drift: arxiv.org/abs/2307.03846 -> "JWST-MIRI spectra of four disks, two compact and two large with multiple radial gaps, selected to test the scenario that water vapor inside the snowline is regulated by pebble drift. [...] These spectra clearly reveal excess emission in the low-energy lines in compact disks, compared to the large disks, establishing the presence of a cooler component with T≈ 170-400 K".

  14. JWST reveals excess cool water near the #snowline in compact disks, consistent with pebble drift: arxiv.org/abs/2307.03846 -> "JWST-MIRI spectra of four disks, two compact and two large with multiple radial gaps, selected to test the scenario that water vapor inside the snowline is regulated by pebble drift. [...] These spectra clearly reveal excess emission in the low-energy lines in compact disks, compared to the large disks, establishing the presence of a cooler component with T≈ 170-400 K".

  15. JWST reveals excess cool water near the #snowline in compact disks, consistent with pebble drift: arxiv.org/abs/2307.03846 -> "JWST-MIRI spectra of four disks, two compact and two large with multiple radial gaps, selected to test the scenario that water vapor inside the snowline is regulated by pebble drift. [...] These spectra clearly reveal excess emission in the low-energy lines in compact disks, compared to the large disks, establishing the presence of a cooler component with T≈ 170-400 K".