16 research outputs found

    Guest-editor Tenzing Gyazu Sherpa: a Profile

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    Polythermal structure of a Himalayan debris-covered glacier revealed by borehole thermometry

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    Runoff from high-elevation debris-covered glaciers represents a crucial water supply for millions of people in the Hindu Kush-Himalaya region, where peak water has already passed in places. Knowledge of glacier thermal regime is essential for predicting dynamic and geometric responses to mass balance change and determining subsurface drainage pathways, which ultimately influence proglacial discharge and hence downstream water availability. Yet, deep internal ice temperatures of these glaciers are unknown, making projections of their future response to climate change highly uncertain. Here, we show that the lower part of the ablation area of Khumbu Glacier, a high-elevation debris-covered glacier in Nepal, may contain ~56% temperate ice, with much of the colder shallow ice near to the melting-point temperature (within 0.8 °C). From boreholes drilled in the glacier’s ablation area, we measured a minimum ice temperature of −3.3 °C, and even the coldest ice we measured was 2 °C warmer than the mean annual air temperature. Our results indicate that high-elevation Himalayan glaciers are vulnerable to even minor atmospheric warming

    A case study using 2019 pre-monsoon snow and stream chemistry in the Khumbu region, Nepal

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    This case study provides a framework for future monitoring and evidence for human source pollution in the Khumbu region, Nepal. We analyzed the chemical composition (major ions, major/trace elements, black carbon, and stable water isotopes) of pre-monsoon stream water (4300–5250 m) and snow (5200–6665 m) samples collected from Mt. Everest, Mt. Lobuche, and the Imja Valley during the 2019 pre-monsoon season, in addition to a shallow ice core recovered from the Khumbu Glacier (5300 m). In agreement with previous work, pre-monsoon aerosol deposition is dominated by dust originating from western sources and less frequently by transport from southerly air mass sources as demonstrated by evidence of one of the strongest recorded pre-monsoon events emanating from the Bay of Bengal, Cyclone Fani. Elevated concentrations of human-sourced metals (e.g., Pb, Bi, As) are found in surface snow and stream chemistry collected in the Khumbu region. As the most comprehensive case study of environmental chemistry in the Khumbu region, this research offers sufficient evidence for increased monitoring in this watershed and surrounding areas

    Characterization of CAP5.5 and CAP5.5V, atypical calpains in Trypanosoma brucei

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    Calpains are a group of calcium-dependent cysteine proteases with roles ranging from cytoskeletal remodelling to signal transduction. In Trypanosoma brucei, the causal agent of African sleeping sickness, an unusually large number of calpain- like proteins exist, whose functions remain unknown. Recently, the procyclic form- specific cytoskeleton associated protein 5.5 (CAP5.5) and its bloodstream-specific paralogous variant, CAP5.5V were discovered to be essential for the proper morphogenesis of the parasite. However, precise functional roles of these proteins remain unknown. In this MSc thesis, I employed a two-pronged approach combining cell biology studies of CAP5.5 and CAP5.5V in T. brucei with in vitro assays of recombinant calpains expressed in Escherichia coli to further characterize CAP5.5 and CAP5.5V. To resolve whether the function of CAP5.5 and CAP5.5V is dependent upon proteolytic activity, I expressed and purified recombinant CAP5.5V’s catalytic domain. I demonstrated that this domain did not have any detectable autolytic activity or activity against universal protease substrates such as casein. Ectopic expression of CAP5.5::YFP::Ty in procyclic trypanosomes led to nuclear mis-positioning among other morphological defects. Additionally, I demonstrated a cell cycle dependency on incorporation of CAP5.5::YFP::Ty into the cytoskeleton and corroborate previous data that suggest that CAP5.5 is built in from the dynamic, posterior end of the cell. Investigation of the molecular determinants in CAP5.5’s sequence such as motifs or domains suggested that CAP5.5’s domain IV may be the domain mediating association with the sub-pellicular cytoskeleton.This thesis is not currently available in ORA

    The Mozart Effect & The Arousal Mood Hypothesis

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    The present study investigated whether performing various musical and non-music activities could induce enhancements to spatial reasoning skills and whether these enhancements could be attributed to changes in arousal and mood. We were able to successfully reproduce the Mozart Effect by showing that subjects in three of our experimental groups exhibited a significant increase in PF&C scores compared to the control group. However, the groups did not show reliable changes in the subjects’ emotional states. Taken together, our results suggest that the enhancements to spatial-reasoning involved in the Mozart Effect may not be attributed to changes in arousal and mood

    The influence of water percolation through crevasses on the thermal regime of a Himalayan mountain glacier

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    In cold and arid climates, small glaciers with cold accumulation zones are often thought to be entirely cold based. However, scattering in ground-penetrating radar (GPR) measurements on the Rikha Samba Glacier in the Nepal Himalayas suggests a large amount of temperate ice that seems to be influenced by the presence of crevassed areas. We used a coupled thermo-mechanical model forced by a firn model accounting for firn heating to interpret the observed thermal regime. Using a simple energy conservation approach, we show that the addition of water percolation and refreezing in crevassed areas explains these observations. Model experiments show that both steady and transient thermal regimes are significantly affected by latent heat release in crevassed areas. This makes half of the glacier base temperate, resulting in an ice dynamic mainly controlled by basal friction instead of ice deformation. The timescale of thermal regime change, in response to atmospheric warming, is also greatly diminished, with a potential switch from cold to temperate basal ice in 50–60 years in the upper part of the glacier instead of the 100–150 years that it would take without the effect of the crevasses. This study highlights the crucial role of water percolation through the crevasses on the thermal regime of glaciers and validates a simple method to account for it in glacier thermo-mechanical models
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