Ginot Patrick, Dumont M., Lim S., Patris Nicolas, Taupin Jean-Denis, Wagnon Patrick, Gilbert A., Arnaud Yves, Marinoni A., Bonasoni P., Laj P. (2014). A 10 year record of black carbon and dust from a Mera Peak ice core (Nepal) : variability and potential impact on melting of Himalayan glaciers. Cryosphere, 8 (4), p. 1479-1496. ISSN 1994-0416.
Titre du document
A 10 year record of black carbon and dust from a Mera Peak ice core (Nepal) : variability and potential impact on melting of Himalayan glaciers
Année de publication
2014
Auteurs
Ginot Patrick, Dumont M., Lim S., Patris Nicolas, Taupin Jean-Denis, Wagnon Patrick, Gilbert A., Arnaud Yves, Marinoni A., Bonasoni P., Laj P.
Source
Cryosphere, 2014,
8 (4), p. 1479-1496 ISSN 1994-0416
A shallow ice core was extracted at the summit of Mera Peak at 6376ma.s.l. in the southern flank of the Nepalese Himalaya range. From this core, we reconstructed the seasonal deposition fluxes of dust and refractory black carbon (rBC) since 1999. This archive presents well preserved seasonal cycles based on a monsoonal precipitation pattern. According to the seasonal precipitation regime in which 80% of annual precipitation falls between June and September, we estimated changes in the concentrations of these aerosols in surface snow. The analyses revealed that mass fluxes are a few orders of magnitude higher for dust (10.4 +/- 2.8 gm(-2) yr(-1)) than for rBC (7.9 +/- 2.8 mgm(-2) yr(-1)). The relative lack of seasonality in the dust record may reflect a high background level of dust inputs, whether from local or regional sources. Over the 10-year record, no deposition flux trends were detected for any of the species of interest. The data were then used to simulate changes in the surface snow albedo over time and the potential melting caused by these impurities. Mean potential melting caused by dust and rBC combined was 713 kgm(-2) yr(-1), and for rBC alone, 342 kgm(-2) yr(-1) for rBC under certain assumptions. Compared to the melting rate measured using the mass and energy balance at 5360ma.s.l. on Mera Glacier between November 2009 and October 2010, i.e. 3000 kgm(-2) yr(-1) and 3690 kgm(-2) yr(-1) respectively, the impact of rBC represents less than 16% of annual potential melting while the contribution of dust and rBC combined to surface melting represents a maximum of 26 %. Over the 10-year period, rBC variability in the ice core signal primarily reflected variability of the monsoon signal rather than variations in the intensity of emissions.
Plan de classement
Sciences du milieu [021]
;
Hydrologie [062]
Description Géographique
NEPAL
Localisation
Fonds IRD [F B010062568]
Identifiant IRD
fdi:010062568
