A platform for research: civil engineering, architecture and urbanism
A platform for research: civil engineering, architecture and urbanism
Climate effect of black carbon aerosol in a Tibetan Plateau glacier
https://orcid.org/0000-0002-8418-0808
https://orcid.org/0000-0001-5212-437X
Abstract In the Tibetan Plateau, the black carbon (BC) concentration in surface snow and snow pits has received much attention, whereas the seasonal behavior of aerosol-in-snow concentration, vertical profile, melt-scavenging, and enrichment have received relatively little attention. Here we investigate these processes and their impacts on radiative forcing on the Muji glacier in the westernmost Tibetan Plateau during the 2012 snowmelt season. Increasing impurity concentrations were mostly due to post-deposition effects rather than new deposition. On 5 July, BC concentrations in the surface snow were higher than those of fresh snow, implying enrichment via sublimation and/or melting of previous snow. Fresh snow contained 25 ng g−1 BC on 27 July; afterward, BC gradually increased, reaching 730.6 ng g−1 in September. BC, organic carbon (OC), and dust concentrations co-varied but differed in magnitude. Melt-scavenging efficiencies were estimated at 0.19 ± 0.05 and 0.04 ± 0.01 for OC and BC, respectively, and the BC in surface snow increased by 20–25 times depending on melt intensity. BC-in-snow radiative forcing (RF) was approximately 2.2 W m−2 for fresh snow and 18.1–20.4 W m−2 for aged snow, and was sometimes reduced by the presence of dust.
Highlights We sampled surface snow and snow pits in the snowmelt season in a Tibetan glacier. We depicted the variability of BC, OC, and dust concentrations. Scavenging efficiency and enrichment for BC and OC were derived. We evaluated BC radiative forcing in snow using SNICAR.
Climate effect of black carbon aerosol in a Tibetan Plateau glacier
https://orcid.org/0000-0002-8418-0808
https://orcid.org/0000-0001-5212-437X
Abstract In the Tibetan Plateau, the black carbon (BC) concentration in surface snow and snow pits has received much attention, whereas the seasonal behavior of aerosol-in-snow concentration, vertical profile, melt-scavenging, and enrichment have received relatively little attention. Here we investigate these processes and their impacts on radiative forcing on the Muji glacier in the westernmost Tibetan Plateau during the 2012 snowmelt season. Increasing impurity concentrations were mostly due to post-deposition effects rather than new deposition. On 5 July, BC concentrations in the surface snow were higher than those of fresh snow, implying enrichment via sublimation and/or melting of previous snow. Fresh snow contained 25 ng g−1 BC on 27 July; afterward, BC gradually increased, reaching 730.6 ng g−1 in September. BC, organic carbon (OC), and dust concentrations co-varied but differed in magnitude. Melt-scavenging efficiencies were estimated at 0.19 ± 0.05 and 0.04 ± 0.01 for OC and BC, respectively, and the BC in surface snow increased by 20–25 times depending on melt intensity. BC-in-snow radiative forcing (RF) was approximately 2.2 W m−2 for fresh snow and 18.1–20.4 W m−2 for aged snow, and was sometimes reduced by the presence of dust.
Highlights We sampled surface snow and snow pits in the snowmelt season in a Tibetan glacier. We depicted the variability of BC, OC, and dust concentrations. Scavenging efficiency and enrichment for BC and OC were derived. We evaluated BC radiative forcing in snow using SNICAR.
Climate effect of black carbon aerosol in a Tibetan Plateau glacier
https://orcid.org/0000-0002-8418-0808
https://orcid.org/0000-0001-5212-437X
Abstract In the Tibetan Plateau, the black carbon (BC) concentration in surface snow and snow pits has received much attention, whereas the seasonal behavior of aerosol-in-snow concentration, vertical profile, melt-scavenging, and enrichment have received relatively little attention. Here we investigate these processes and their impacts on radiative forcing on the Muji glacier in the westernmost Tibetan Plateau during the 2012 snowmelt season. Increasing impurity concentrations were mostly due to post-deposition effects rather than new deposition. On 5 July, BC concentrations in the surface snow were higher than those of fresh snow, implying enrichment via sublimation and/or melting of previous snow. Fresh snow contained 25 ng g−1 BC on 27 July; afterward, BC gradually increased, reaching 730.6 ng g−1 in September. BC, organic carbon (OC), and dust concentrations co-varied but differed in magnitude. Melt-scavenging efficiencies were estimated at 0.19 ± 0.05 and 0.04 ± 0.01 for OC and BC, respectively, and the BC in surface snow increased by 20–25 times depending on melt intensity. BC-in-snow radiative forcing (RF) was approximately 2.2 W m−2 for fresh snow and 18.1–20.4 W m−2 for aged snow, and was sometimes reduced by the presence of dust.
Highlights We sampled surface snow and snow pits in the snowmelt season in a Tibetan glacier. We depicted the variability of BC, OC, and dust concentrations. Scavenging efficiency and enrichment for BC and OC were derived. We evaluated BC radiative forcing in snow using SNICAR.
Climate effect of black carbon aerosol in a Tibetan Plateau glacier
Yang, Song (author) / Xu, Baiqing (author) / Cao, Junji (author) / Zender, Charles S. (author) / Wang, Mo (author)
Atmospheric Environment ; 111 ; 71-78
2015-03-09
8 pages
Article (Journal)
Electronic Resource
English
Climate effect of black carbon aerosol in a Tibetan Plateau glacier
| Elsevier | 2015
Measurements of Glacier Variation in the Tibetan Plateau Using Landsat Data
| Online Contents | 1998
Different characteristics of two surges in Weigeledangxiong Glacier, northeastern Tibetan Plateau
| DOAJ | 2022
Three-Dimensional Glacier Changes in Geladandong Peak Region in the Central Tibetan Plateau
| DOAJ | 2018