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Manuscript Type: Empirical Research Question/Issue: Why do firms in China, which has a higher level of economic development, communicate less CSR than firms in India? We use a model that includes country-, industry-, and firm-level factors to predict CSR communications intensity, a proxy for CSR activities. Research Findings/Insights: Using data on 68 of the largest multinational companies in China and India, our study shows that Indian firms communicate more CSR primarily due to a more rule-based, as opposed to relation-based, governance environment. Firms in the manufacturing industry tend to communicate more CSR. Firm-level characteristics such as size, duality of CEO and board chairperson, and percentage of external members on the board also have a significant influence on CSR communications. Theoretical/ Academic Implications: The main theoretical contribution of our study is to bring a three-level perspective, relying not only on firm- and industry-specific factors, but also on the governance environment, to the study of firms' CSR behavior. We show that the national governance environment dominates the national income level in affecting CSR communications intensity. We demonstrate that the macro institutional environment in a country strongly affects firm CSR behavior. Our findings suggest that CSR should be studied by considering multilevel antecedents. Practitioner/Policy Implications: Our study suggests that in order to improve the CSR of firms, policy makers in India and China must first try to improve public governance at the national level. Executives doing business with Chinese and Indian companies need to better understand the contrasting governance and their effects on the CSR practices in each country. For the international community and those concerned about product safety and other social issues related to China and India, our findings suggest that improvement will not be immediate since the governance environment changes relatively slowly.
A lasting legacy of the International Polar Year (IPY) 2007–2008 was the promotion of the Permafrost Young Researchers Network (PYRN), initially an IPY outreach and education activity by the International Permafrost Association (IPA). With the momentum of IPY, PYRN developed into a thriving network that still connects young permafrost scientists, engineers, and researchers from other disciplines. This research note summarises (1) PYRN’s development since 2005 and the IPY’s role, (2) the first 2015 PYRN census and survey results, and (3) PYRN’s future plans to improve international and interdisciplinary exchange between young researchers. The review concludes that PYRN is an established network within the polar research community that has continually developed since 2005. PYRN’s successful activities were largely fostered by IPY. With >200 of the 1200 registered members active and engaged, PYRN is capitalising on the availability of social media tools and rising to meet environmental challenges while maintaining its role as a successful network honouring the legacy of IPY.
A local and flexible definition of the monsoon season based on hydrological evidence is important for the understanding and management of Himalayan water resources. Here, we present an objective statistical method to retrieve seasonal hydrometeorological transitions. Applied to daily rainfall data (1951-2015), this method shows an average longitudinal delay of similar to 15 days, with later monsoon onset and earlier withdrawal in the western Himalaya, consistent with the continental progression of wet air masses. This delay leads to seasons of different length along the Himalaya and biased precipitation amounts when using uniform calendric monsoon boundaries. In the Central Himalaya annual precipitation has increased, due primarily to an increase of premonsoon precipitation. These findings highlight issues associated with a static definition of monsoon boundaries and call for a deeper understanding of nonmonsoonal precipitation over the Himalayan water tower. <br /> Plain Language Summary Precipitation in the Himalayas determines water availability for the Indian foreland with large socioeconomic implications. Despite its importance, spatial and temporal patterns of precipitation are poorly understood. Here, we estimate the long-term average and trends of seasonal precipitation at the scale of individual catchments draining the Himalayas. We apply a statistical method to detect the timing of hydrometeorological seasons from local precipitation measurements, focusing on monsoon onset and withdrawal. We identify longitudinal and latitudinal delays, resulting in seasons of different length along and across the Himalayas. These spatial patterns and the annual variability of the monsoon boundaries mean that oft-used, fixed calendric dates, for example, 1 June to 30 September, may be inadequate for retrieving monsoon rainfall totals. Moreover, we find that, despite its prominent contribution to annual rainfall totals, the Indian summer monsoon cannot explain the increase of the annual precipitation over the Central Himalayas. Instead, this appears to be mostly driven by changes in premonsoon and winter rainfall. So far, little attention has been paid to premonsoon precipitation, but governed by evaporative processes and surface water availability, it may be enhanced by irrigation and changed land use in the Gangetic foreland.