We find evidence that black soot aerosols deposited on Tibetan glaciers have been a significant contributing factor to observed rapid glacier retreat. Reduced black soot emissions, in addition to reduced greenhouse gases, may be required to avoid demise of Himalayan glaciers and retain the benefits of glaciers for seasonal fresh water supplies.aerosols ͉ climate change ͉ fresh water ͉ glacier retreat ͉ Tibetan Plateau

Mesenchymal stem cells (MSCs) have been used experimentally for treating inflammatory disorders, partly due to their immunosuppressive properties. Although interleukin-1b (IL-1b) is one of the most important inflammatory mediators, growing evidence indicates that IL-1b signaling elicits the immunosuppressive properties of MSCs. However, it remains unclear how IL-1b signaling accomplishes this activity. Here, we focus on the therapeutic efficacy of IL-1b-primed MSCs in the dextran sulfate sodium (DSS)-induced colitis model, in addition to the underlining mechanisms. We first found that IL-1b-primed MSCs, without any observable phenotype change in vitro, significantly attenuated the development of DSS-induced murine colitis. Moreover, IL-1b-primed MSCs modulated the balance of immune cells in the spleen and the mesenteric lymph nodes (MLNs) through elevating cyclooxygenase-2 (COX-2), IL-6 and IL-8 expression and influencing the polarization of peritoneal macrophages. Importantly, IL-1b-primed MSCs possessed an enhanced ability to migrate to the inflammatory site of the gut via upregulation of chemokine receptor type 4 (CXCR4) expression. In summary, IL-1b-primed MSCs have improved efficacy in treating DSS-induced colitis, which at least partly depends on their increased immunosuppressive capacities and enhanced migration ability.

The post-depositional enrichment of black soot in snow-pack was investigated by measuring the redistribution of black soot along monthly snow-pits on a Tien Shan glacier. The one-year experiment revealed that black soot was greatly enriched, defined as the ratio of concentration to original snow concentration, in the unmelted snow-pack by at least an order of magnitude. Greatest soot enrichment was observed in the surface snow and the lower firn-pack within the melt season percolation zone. Black carbon (BC) concentrations as high as 400 ng g −1 in the summer surface snow indicate that soot can significantly contribute to glacier melt. BC concentrations reaching 3000 ng g −1 in the bottom portion of the firn pit are especially concerning given the expected equilibrium-line altitude (ELA) rise associated with future climatic warming, which would expose the dirty underlying firn and ice. Since most of the accumulation area on Tibetan glaciers is within the percolation zone where snow densification is characterized by melting and refreezing, the enrichment of black soot in the snow-pack is of foremost importance. Results suggest the effect of black soot on glacier melting may currently be underestimated.