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1. Understanding Open Defecation in the Age of Swachh Bharat Abhiyan: Agency, Accountability, and Anger in Rural Bihar

   https://doi.org/10.3390/ijerph17041384  

   Jain, Anoop; Wagner, Ashley; Snell-Rood, Claire; Ray, Isha (February 2020, International Journal of Environmental Research and Public Health)

   null (Ed.)

   Swachh Bharat Abhiyan, India’s flagship sanitation intervention, set out to end open defecation by October 2019. While the program improved toilet coverage nationally, large regional disparities in construction and use remain. Our study used ethnographic methods to explore perspectives on open defecation and latrine use, and the socio-economic and political reasons for these perspectives, in rural Bihar. We draw on insights from social epidemiology and political ecology to explore the structural determinants of latrine ownership and use. Though researchers have often pointed to rural residents’ preference for open defecation, we found that people were aware of its many risks. We also found that (i) while sanitation research and “behavior change” campaigns often conflate the reluctance to adopt latrines with a preference for open defecation, this is an erroneous conflation; (ii) a subsidy can help (some) households to construct latrines but the amount of the subsidy and the manner of its disbursement are key to its usefulness; and (iii) widespread resentment towards what many rural residents view as a development bias against rural areas reinforces distrust towards the government overall and its Swachh Bharat Abhiyan-funded latrines in particular. These social-structural explanations for the slow uptake of sanitation in rural Bihar (and potentially elsewhere) deserve more attention in sanitation research and promotion efforts. 

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2. Soil and plant variables collected at brown lemming structure sites near Utqaigvik, Alaska, summer 2021

   https://doi.org/10.18739/A2GX44W4K  

   Roy, Austin; McLaren, Jennie (June 2022, NSF Arctic Data Center)

   This data describes above-ground and below-ground variables collected under small mammal-built structures and control sites from two tundra locations in polygonal tundra near Utqiagvik, Alaska, USA. Small mammal structures sampled included hay piles (winter nests), runways, latrines, and burrow entrances. Above-ground data collected include relative percent cover, litter depth, and Normalized Difference Vegetation Index. Below-ground data collected include inorganic soil nutrients, total extractable soil nutrients, microbial biomass nutrients, microbial exo-enzyme activities, soil pH, soil conductivity, soil temperature, and soil respiration. 

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3. Small but mighty: Impacts of rodent‐herbivore structures on carbon and nutrient cycling in arctic tundra

   https://doi.org/10.1111/1365-2435.14127  

   Roy, Austin; Gough, Laura; Boelman, Natalie T.; Rowe, Rebecca J.; Griffin, Kevin L.; McLaren, Jennie R. (July 2022, Functional Ecology)

   Abstract Understanding arctic ecosystem function is key to understanding future global carbon (C) and nutrient cycling processes. However, small mammal herbivores can have effects on ecosystems as structure builders and these effects have been underrepresented in the understanding of arctic systems.We examined the impact of small mammal structures (hay piles, runways, latrines) on soils and plants in three arctic tundra regions near Utqiaġvik, Toolik Lake, and Nome, Alaska. Our aims were to (1) examine how vole and lemming structures influence plant and soil nutrient pools and microbial processes, (2) determine if structure effects were similar across tundra system types, and (3) understand how changes in the abundance and cover of these structures during different phases of small mammal multi‐annual population cycles might influence biogeochemical cycling.In general, small mammal structures increased nitrogen (N) availability in soils, although effects varied by study region. Across study regions, hay piles were relatively uncommon (lowest % cover) but increased multiple soil N and P pools, C‐ and N‐acquiring enzyme activities, and leaf phosphorus (P) concentrations, with the specific nutrient variables and size of the effects varying by study region. Latrines had the second highest cover and influenced multiple C, N and P pools, but their effects were mainly observed within a single region. Lastly, runways had the highest % cover of all activity types but increased the fewest number of soil nutrient variables.We conclude that by influencing soil nutrient availability and biogeochemical cycling, small mammal structures can influence bottom‐up regulation of ecosystem function, particularly during the high phase of the small mammal population cycle. Future changes in these population cycles might alter the role of small mammals in the Arctic and have lasting effects on system processes. Read the freePlain Language Summaryfor this article on the Journal blog 

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4. Meteorological and geographical factors associated with dry lightning in central and northern California

   https://doi.org/10.1088/2752-5295/ac84a0  

   Kalashnikov, Dmitri A.; Abatzoglou, John T.; Nauslar, Nicholas J.; Swain, Daniel L.; Touma, Danielle; Singh, Deepti (August 2022, Environmental Research: Climate)

   Abstract Lightning occurring with less than 2.5 mm of rainfall—typically referred to as ‘dry lightning’—is a major source of wildfire ignition in central and northern California. Despite being rare, dry lightning outbreaks have resulted in destructive fires in this region due to the intersection of dense, dry vegetation and a large population living adjacent to fire-prone lands. Since thunderstorms are much less common in this region relative to the interior West, the climatology and drivers of dry lightning have not been widely investigated in central and northern California. Using daily gridded lightning and precipitation observations (1987–2020) in combination with atmospheric reanalyses, we characterize the climatology of dry lightning and the associated meteorological conditions during the warm season (May–October) when wildfire risk is highest. Across the domain, nearly half (∼46%) of all cloud-to-ground lightning flashes occurred as dry lightning during the study period. We find that higher elevations (>2000 m) receive more dry lightning compared to lower elevations (<1000 m) with activity concentrated in July-August. Although local meteorological conditions show substantial spatial variation, we find regionwide enhancements in mid-tropospheric moisture and instability on dry lightning days relative to background climatology. Additionally, surface temperatures, lower-tropospheric dryness, and mid-tropospheric instability are increased across the region on dry versus wet lightning days. We also identify widespread dry lightning outbreaks in the historical record, quantify their seasonality and spatial extent, and analyze associated large-scale atmospheric patterns. Three of these four atmospheric patterns are characterized by different configurations of ridging over the continental interior and offshore troughing. Understanding the meteorology of dry lightning across this region can inform forecasting of possible wildfire ignitions and is relevant for assessing changes in dry lightning and wildfire risk in climate projections. 

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5. Importance of dry deposition parameterization choice in global simulations of surface ozone

   https://doi.org/10.5194/acp-19-14365-2019  

   Wong, Anthony Y.; Geddes, Jeffrey A.; Tai, Amos P.; Silva, Sam J. (January 2019, Atmospheric Chemistry and Physics)

   Abstract. Dry deposition is a major sink of tropospheric ozone.Increasing evidence has shown that ozone dry deposition actively linksmeteorology and hydrology with ozone air quality. However, there is littlesystematic investigation on the performance of different ozone drydeposition parameterizations at the global scale and how parameterizationchoice can impact surface ozone simulations. Here, we present the results ofthe first global, multidecadal modelling and evaluation of ozone drydeposition velocity (vd) using multiple ozone dry depositionparameterizations. We model ozone dry deposition velocities over 1982–2011using four ozone dry deposition parameterizations that are representative ofcurrent approaches in global ozone dry deposition modelling. We useconsistent assimilated meteorology, land cover, and satellite-derived leafarea index (LAI) across all four, such that the differences in simulatedvd are entirely due to differences in deposition model structures orassumptions about how land types are treated in each. In addition, we usethe surface ozone sensitivity to vd predicted by a chemical transportmodel to estimate the impact of mean and variability of ozone dry depositionvelocity on surface ozone. Our estimated vd values from four differentparameterizations are evaluated against field observations, and whileperformance varies considerably by land cover types, our results suggestthat none of the parameterizations are universally better than the others.Discrepancy in simulated mean vd among the parameterizations isestimated to cause 2 to 5 ppbv of discrepancy in surface ozone in theNorthern Hemisphere (NH) and up to 8 ppbv in tropical rainforests in July,and up to 8 ppbv in tropical rainforests and seasonally dry tropical forestsin Indochina in December. Parameterization-specific biases based onindividual land cover type and hydroclimate are found to be the two maindrivers of such discrepancies. We find statistically significant trends inthe multiannual time series of simulated July daytime vd in allparameterizations, driven by warming and drying (southern Amazonia, southernAfrican savannah, and Mongolia) or greening (high latitudes). The trend inJuly daytime vd is estimated to be 1 % yr−1 and leadsto up to 3 ppbv of surface ozone changes over 1982–2011. The interannual coefficient ofvariation (CV) of July daytime mean vd in NH is found to be5 %–15 %, with spatial distribution that varies with the dry depositionparameterization. Our sensitivity simulations suggest this can contributebetween 0.5 to 2 ppbv to interannual variability (IAV) in surface ozone, butall models tend to underestimate interannual CV when compared to long-termozone flux observations. We also find that IAV in some dry depositionparameterizations is more sensitive to LAI, while in others it is more sensitiveto climate. Comparisons with other published estimates of the IAV ofbackground ozone confirm that ozone dry deposition can be an important partof natural surface ozone variability. Our results demonstrate the importanceof ozone dry deposition parameterization choice on surface ozone modellingand the impact of IAV of vd on surface ozone, thus making a strong casefor further measurement, evaluation, and model–data integration of ozone drydeposition on different spatiotemporal scales. 

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