[1] Particle number size distributions between 3 nm and 10 mm were measured in Beijing, China. New particle formation events were observed on around 40% of the measurement days from March 2004 to February 2005 and were generally observed under low relative humidity and sunny conditions. Though occurring during all seasons, new particle formation events had highest frequency in spring and lowest frequency in summer. Events were classified as ''clean'' or ''polluted'' groups mainly according to the condensational sink and the local wind. The formation rate range was from 3.3 to 81.4 cm À3 s À1 . The growth rate varied from 0.1 to 11.2 nm h À1. The seasonal variation of condensable vapor concentration showed the highest values during summer months due to enhanced photochemical and biological activities as well as stagnant air masses preventing exchange with cleaner air.

In the quest for a functional cure or eradication of HIV infection, we need to know how large the reservoirs are from which infection rebounds when treatment is interrupted. To that end, we quantified SIV and HIV tissue burdens in tissues of infected non-human primates and lymphoid tissue (LT) biopsies from infected humans. Before antiretroviral therapy (ART), LTs harbor more than 98 percent of the SIV RNA+ and DNA+ cells. While ART substantially reduced their numbers, vRNA+ cells were still detectable and their persistence was associated with relatively low drug concentrations in LT compared to peripheral blood. Prolonged ART also reduced the level of SIV and HIV-DNA+ cells, but the estimated size of the residual tissue burden of 108 vDNA+ cells that potentially harbor replication competent proviruses, along with the evidence for continuing virus production in LT despite ART, identify two important sources for rebound following treatment interruption. The large sizes of these tissue reservoirs underscore the challenges in developing “HIV cure” strategies that target multiple sources of virus production.

Black carbon (BC) and light-absorbing organic carbon (brown carbon, BrC) play key roles in warming the atmosphere, but the magnitude of their effects remains highly uncertain. Theoretical modelling and laboratory experiments demonstrate that coatings on BC can enhance BC's light absorption, therefore many climate models simply assume enhanced BC absorption by a factor of ∼1.5. However, recent field observations show negligible absorption enhancement, implying models may overestimate BC's warming. Here we report direct evidence of substantial field-measured BC absorption enhancement, with the magnitude strongly depending on BC coating amount. Increases in BC coating result from a combination of changing sources and photochemical aging processes. When the influence of BrC is accounted for, observationally constrained model calculations of the BC absorption enhancement can be reconciled with the observations. We conclude that the influence of coatings on BC absorption should be treated as a source and regionally specific parameter in climate models.