Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire

Assessing the potential for black carbon (BC) and dust deposition to reduce albedo and accelerate glacier melt is of interest in Washington because snow and glacier melt are an important source of water resources, and glaciers are retreating. In August 2012 on Snow Dome, Mount Olympus, Washington, w...

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Main Authors: Kaspari, Susan, Skiles, S. McKenzie, Delaney, Ian, Dixon, Daniel
Format: Text
Language:English
Published: ScholarWorks@CWU 2015
Subjects:
Online Access:https://digitalcommons.cwu.edu/geological_sciences/25
https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1025&context=geological_sciences
id ftcwashingtonuni:oai:digitalcommons.cwu.edu:geological_sciences-1025
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spelling ftcwashingtonuni:oai:digitalcommons.cwu.edu:geological_sciences-1025 2023-05-15T16:38:59+02:00 Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire Kaspari, Susan Skiles, S. McKenzie Delaney, Ian Dixon, Daniel 2015-01-01T08:00:00Z application/pdf https://digitalcommons.cwu.edu/geological_sciences/25 https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1025&context=geological_sciences English eng ScholarWorks@CWU https://digitalcommons.cwu.edu/geological_sciences/25 https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1025&context=geological_sciences Geological Sciences Faculty Scholarship glacier melt black carbon deposition Mount Olympus Washington Geology text 2015 ftcwashingtonuni 2022-10-20T20:26:58Z Assessing the potential for black carbon (BC) and dust deposition to reduce albedo and accelerate glacier melt is of interest in Washington because snow and glacier melt are an important source of water resources, and glaciers are retreating. In August 2012 on Snow Dome, Mount Olympus, Washington, we measured snow surface spectral albedo and collected surface snow samples and a 7 m ice core. The snow and ice samples were analyzed for iron (Fe, used as a dust proxy) via inductively coupled plasma sector field mass spectrometry, total impurity content gravimetrically, BC using a single-particle soot photometer (SP2), and charcoal through microscopy. In the 2012 summer surface snow, BC (54 ± 50 μg/L), Fe (367±236 μg/L) and gravimetric impurity (35 ± 18 mg/L) concentrations were spatially variable, and measured broadband albedo varied between 0.67–0.74. BC and dust concentrations in the ice core 2011 summer horizon were a magnitude higher (BC = 3120 μg/L, Fe = 22000 μg/L, and gravimetric impurity = 1870 mg/L), corresponding to a modeled broadband albedo of 0.45 based on the measured BC and ravimetric impurity concentrations. The Big Hump forest fire is the likely source for the higher concentrations. Modeling constrained by measurements indicates that the all-sky 12 h daily mean radiative forcings in summer 2012 and 2011 range between 37–53Wm_2 and 112–149Wm_2, respectively, with the greater forcings in 2011 corresponding to a 29–38mm/d enhancement in snowmelt. The timing of the forest fire impurity deposition is coincident with an increase in observed discharge in the Hoh River, highlighting the potential for BC and dust deposition on glaciers from forest fires to accelerate melt. Text ice core Central Washington University: ScholarWorks Mount Olympus ENVELOPE(162.000,162.000,-77.467,-77.467) Olympus ENVELOPE(156.767,156.767,-80.217,-80.217) Snow Dome ENVELOPE(-89.967,-89.967,79.435,79.435)
institution Open Polar
collection Central Washington University: ScholarWorks
op_collection_id ftcwashingtonuni
language English
topic glacier melt
black carbon deposition
Mount Olympus
Washington
Geology
spellingShingle glacier melt
black carbon deposition
Mount Olympus
Washington
Geology
Kaspari, Susan
Skiles, S. McKenzie
Delaney, Ian
Dixon, Daniel
Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire
topic_facet glacier melt
black carbon deposition
Mount Olympus
Washington
Geology
description Assessing the potential for black carbon (BC) and dust deposition to reduce albedo and accelerate glacier melt is of interest in Washington because snow and glacier melt are an important source of water resources, and glaciers are retreating. In August 2012 on Snow Dome, Mount Olympus, Washington, we measured snow surface spectral albedo and collected surface snow samples and a 7 m ice core. The snow and ice samples were analyzed for iron (Fe, used as a dust proxy) via inductively coupled plasma sector field mass spectrometry, total impurity content gravimetrically, BC using a single-particle soot photometer (SP2), and charcoal through microscopy. In the 2012 summer surface snow, BC (54 ± 50 μg/L), Fe (367±236 μg/L) and gravimetric impurity (35 ± 18 mg/L) concentrations were spatially variable, and measured broadband albedo varied between 0.67–0.74. BC and dust concentrations in the ice core 2011 summer horizon were a magnitude higher (BC = 3120 μg/L, Fe = 22000 μg/L, and gravimetric impurity = 1870 mg/L), corresponding to a modeled broadband albedo of 0.45 based on the measured BC and ravimetric impurity concentrations. The Big Hump forest fire is the likely source for the higher concentrations. Modeling constrained by measurements indicates that the all-sky 12 h daily mean radiative forcings in summer 2012 and 2011 range between 37–53Wm_2 and 112–149Wm_2, respectively, with the greater forcings in 2011 corresponding to a 29–38mm/d enhancement in snowmelt. The timing of the forest fire impurity deposition is coincident with an increase in observed discharge in the Hoh River, highlighting the potential for BC and dust deposition on glaciers from forest fires to accelerate melt.
format Text
author Kaspari, Susan
Skiles, S. McKenzie
Delaney, Ian
Dixon, Daniel
author_facet Kaspari, Susan
Skiles, S. McKenzie
Delaney, Ian
Dixon, Daniel
author_sort Kaspari, Susan
title Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire
title_short Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire
title_full Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire
title_fullStr Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire
title_full_unstemmed Accelerated Glacier Melt on Snow Dome, Mount Olympus, Washington, USA, due to Deposition of Black Carbon and Mineral Dust from Wildfire
title_sort accelerated glacier melt on snow dome, mount olympus, washington, usa, due to deposition of black carbon and mineral dust from wildfire
publisher ScholarWorks@CWU
publishDate 2015
url https://digitalcommons.cwu.edu/geological_sciences/25
https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1025&context=geological_sciences
long_lat ENVELOPE(162.000,162.000,-77.467,-77.467)
ENVELOPE(156.767,156.767,-80.217,-80.217)
ENVELOPE(-89.967,-89.967,79.435,79.435)
geographic Mount Olympus
Olympus
Snow Dome
geographic_facet Mount Olympus
Olympus
Snow Dome
genre ice core
genre_facet ice core
op_source Geological Sciences Faculty Scholarship
op_relation https://digitalcommons.cwu.edu/geological_sciences/25
https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1025&context=geological_sciences
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