FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2948398422> ?p ?o ?g. }

• W2948398422 endingPage "1038" @default.
• W2948398422 startingPage "1030" @default.
• W2948398422 abstract "Black carbon (BC), which consists of the strongest light-absorbing particles (LAP) in snow/ice, has been regarded as a potential factor accelerating the melting of glaciers and snow cover over the Third Pole. During the winter and summer of 2016, snow, ice and topsoil were sampled from the Laohugou basin located on the northeastern Tibetan Plateau. Concentrations of BC in Laohugou Glacier No. 12 (LG12) and snow cover in this basin (LSC) varied broadly (21.7–2700.1 and 89.6 to 6326.2 ng g−1, respectively), indicating large spatiotemporal variability in wet, dry and post depositional conditions. Further, internally mixed BC in snow grains enhanced the albedo reduction (15.0–26.3%) more than externally mixed BC in LG12 and LSC. Dust played a more important role than BC in accelerating the melting of LG12, whereas these components played comparable roles in accelerating the melting of LSC. In total, externally mixed BC and dust reduced the albedo by 0.075–0.423, with an associated mean radiative forcing (RF) of 97.5 ± 41.5 Wm−2 in LSC. This level was lower than those in the ablation zone (354.1 ± 81.2 Wm−2) and accumulation zone (145.6 ± 76.7 Wm−2) of LG12 because of discrepancies in LAP concentrations, solar zenith angles and incoming shortwave radiation. Furthermore, we observed that topsoil containing abundant BC was transported along the slope from the debris to the LG12 surface ice, and topsoil in this region could be lifted by strong mountain-valley winds and then deposited on snow/ice surfaces, which affected the LAP concentrations. Therefore, this study is important for understanding the role of BC and dust in the melting of snow/ice in the northeastern Tibetan Plateau." @default.
• W2948398422 created "2019-06-14" @default.
• W2948398422 creator A5016587571 @default.
• W2948398422 creator A5030691366 @default.
• W2948398422 creator A5034824481 @default.
• W2948398422 creator A5035103195 @default.
• W2948398422 creator A5039005708 @default.
• W2948398422 creator A5042642226 @default.
• W2948398422 creator A5068175005 @default.
• W2948398422 creator A5079702492 @default.
• W2948398422 creator A5082785186 @default.
• W2948398422 creator A5086005303 @default.
• W2948398422 date "2019-10-01" @default.
• W2948398422 modified "2023-10-17" @default.
• W2948398422 title "Black carbon in a glacier and snow cover on the northeastern Tibetan Plateau: Concentrations, radiative forcing and potential source from local topsoil" @default.
• W2948398422 cites W1545342756 @default.
• W2948398422 cites W1817182403 @default.
• W2948398422 cites W1907369419 @default.
• W2948398422 cites W1916920625 @default.
• W2948398422 cites W1966586899 @default.
• W2948398422 cites W1978265846 @default.
• W2948398422 cites W1980344828 @default.
• W2948398422 cites W1982231552 @default.
• W2948398422 cites W1984720241 @default.
• W2948398422 cites W1985078380 @default.
• W2948398422 cites W1987461785 @default.
• W2948398422 cites W1993138195 @default.
• W2948398422 cites W1993847517 @default.
• W2948398422 cites W1994863068 @default.
• W2948398422 cites W1999866891 @default.
• W2948398422 cites W2003296784 @default.
• W2948398422 cites W2003636035 @default.
• W2948398422 cites W2004996508 @default.
• W2948398422 cites W2010882378 @default.
• W2948398422 cites W2022588621 @default.
• W2948398422 cites W2028999185 @default.
• W2948398422 cites W2029109615 @default.
• W2948398422 cites W2029136094 @default.
• W2948398422 cites W2037244406 @default.
• W2948398422 cites W2040224800 @default.
• W2948398422 cites W2041376954 @default.
• W2948398422 cites W2046828512 @default.
• W2948398422 cites W2046994624 @default.
• W2948398422 cites W2051043066 @default.
• W2948398422 cites W2064201423 @default.
• W2948398422 cites W2073806577 @default.
• W2948398422 cites W2081258683 @default.
• W2948398422 cites W2095569738 @default.
• W2948398422 cites W2101335647 @default.
• W2948398422 cites W210143032 @default.
• W2948398422 cites W2110052588 @default.
• W2948398422 cites W2110071165 @default.
• W2948398422 cites W2112500985 @default.
• W2948398422 cites W2113383654 @default.
• W2948398422 cites W2118491483 @default.
• W2948398422 cites W2129409468 @default.
• W2948398422 cites W2137169911 @default.
• W2948398422 cites W2150668626 @default.
• W2948398422 cites W2156730686 @default.
• W2948398422 cites W2160308683 @default.
• W2948398422 cites W2162214076 @default.
• W2948398422 cites W2164990341 @default.
• W2948398422 cites W2170884282 @default.
• W2948398422 cites W2174276022 @default.
• W2948398422 cites W2306712365 @default.
• W2948398422 cites W2334305476 @default.
• W2948398422 cites W2345553416 @default.
• W2948398422 cites W2509324708 @default.
• W2948398422 cites W2513572388 @default.
• W2948398422 cites W2572652682 @default.
• W2948398422 cites W2574467146 @default.
• W2948398422 cites W2587774721 @default.
• W2948398422 cites W2594279578 @default.
• W2948398422 cites W2727453429 @default.
• W2948398422 cites W2735452805 @default.
• W2948398422 cites W2735911236 @default.
• W2948398422 cites W2787324423 @default.
• W2948398422 cites W2789823868 @default.
• W2948398422 cites W2804409222 @default.
• W2948398422 cites W2894618029 @default.
• W2948398422 cites W2920254659 @default.
• W2948398422 cites W2955286355 @default.
• W2948398422 doi "https://doi.org/10.1016/j.scitotenv.2019.05.469" @default.
• W2948398422 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/31200301" @default.
• W2948398422 hasPublicationYear "2019" @default.
• W2948398422 type Work @default.
• W2948398422 sameAs 2948398422 @default.
• W2948398422 citedByCount "27" @default.
• W2948398422 countsByYear W29483984222019 @default.
• W2948398422 countsByYear W29483984222020 @default.
• W2948398422 countsByYear W29483984222021 @default.
• W2948398422 countsByYear W29483984222022 @default.
• W2948398422 countsByYear W29483984222023 @default.
• W2948398422 crossrefType "journal-article" @default.
• W2948398422 hasAuthorship W2948398422A5016587571 @default.
• W2948398422 hasAuthorship W2948398422A5030691366 @default.
• W2948398422 hasAuthorship W2948398422A5034824481 @default.
• W2948398422 hasAuthorship W2948398422A5035103195 @default.

• next