7,462 research outputs found

    Rahul Sankrityayan, Tsetan Phuntsog and Tibetan Textbooks for Ladakh in 1933

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    In 1933 the Indian scholar and social activist Rahul Sankrityayan (1893-1963) compiled a set of four Tibetan-language readers and a grammar for use in Ladakhi schools, together with his Ladakhi colleague Tsetan Phuntsog. The readers contain a mix of material from Western, Indian, Ladakhi and Tibetan sources. This includes simple essays about ‘air’ and ‘water’, selections from Aesop’s fables, Indian folk stories, biographies of famous people in Ladakhi and Tibetan history, poems by Ladakhi authors, and extracts from the Treasury of Elegant Sayings by Sakya Pandita Kunga Gyaltsen (1182-1251). This essay begins with a review of earlier Tibetan-language schoolbooks published in British India, and then discusses the circumstances that led to Sankrityayan’s involvement in the Ladakh project. The second part of the essay examines the contents of the readers and the grammar, including—where possible—the authorship of particular sections. Finally, the essay briefly reviews linguistic developments in Ladakh since the publication of the textbooks

    Classification as Narrative: A Renewed Perspective on a Longstanding Topic in Ethnobiology

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    The present work offers a renewed perspective on natural-kind classification in the field of ethnobiology, one that focuses on analyzing higher-order classifications as a form of narrative. By examining changes in classification of materia medica in three main medical/pharmacological texts from three time periods of the Tibetan medicine tradition, we see an overarching shift in classification from a focus on medical efficacy to one on material substance and morphology, thus suggesting influence from pre-twenty-first century western, Linnaean science. The work then links this historical narrative to the complexities of classification of materia medica among contemporary doctors of Tibetan medicine in the People’s Republic of China, who utilize several classificatory schemata. The work encourages continued research in the area of diachronic classification, particularly in terms of what can be gleaned about cultural, political, and social changes in a tradition

    Rock Glacier Characteristics Under Semiarid Climate Conditions in the Western NyainqĂȘntanglha Range, Tibetan Plateau

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    Abstract Rock glaciers are receiving increased attention as a potential source of water and indicator of climate change in periglacial landscapes. They consist of an ice‐debris mixture, which creeps downslope. Although rock glaciers are a wide‐spread feature on the Tibetan Plateau, characteristics such as its ice fraction are unknown as a superficial debris layer inhibits remote assessments. We investigate one rock glacier in the semiarid western NyainqĂȘntanglha range (WNR) with a multi‐method approach, which combines geophysical, geological and geomorphological field investigations with remote sensing techniques. Long‐term kinematics of the rock glacier are detected by 4‐year InSAR time series analysis. The ice content and the active layer are examined by electrical resistivity tomography, ground penetrating radar, and environmental seismology. Short‐term activity (11‐days) is captured by a seismic network. Clast analysis shows a sorting of the rock glacier's debris. The rock glacier has three zones, which are defined by the following characteristics: (a) Two predominant lithology types are preserved separately in the superficial debris patterns, (b) heterogeneous kinematics and seismic activity, and (c) distinct ice fractions. Conceptually, the studied rock glacier is discussed as an endmember of the glacier—debris‐covered glacier—rock glacier continuum. This, in turn, can be linked to its location on the semiarid lee‐side of the mountain range against the Indian summer monsoon. Geologically preconditioned and glacially overprinted, the studied rock glacier is suggested to be a recurring example for similar rock glaciers in the WNR. This study highlights how geology, topography and climate influence rock glacier characteristics and development.Plain Language Summary Climate change has begun to impact all regions of our planet. In cold regions, such as high‐mountain areas, rising temperatures lead to massive melting of glaciers. Besides this evident loss of ice, permafrost, a long‐term ice resource hidden in the subsurface, has started to thaw. Rock glaciers as visible permafrost‐related landforms consist of an ice‐debris mixture, which makes them creep downslope. Due to this movement and their recognizable shape, rock glaciers are permafrost indicators in high‐mountain areas. We investigate one rock glacier in the western NyaingĂȘntanglha Range (Tibetan Plateau) using field and remote sensing methods to understand its development and to know the current state of its ice core. Our main outcome is, that the heterogeneous creeping behavior, the properties of the debris cover as well as the internal distribution of ice are the results of a continuous development from a glacier into today's rock glacier. In particular, the high ice content in particular sections points to such a glacial precondition. The debris layer covering the internal ice attenuates the effect of climate warming. This makes the rock glacier and similar rock glaciers found in the northern part of the mountain range important future water resources for the semiarid region.Key Points Geophysical and remote sensing methods in concert reveal the morphostructure, ice fraction, and kinematics of the studied rock glacier Rock glacier characteristics are controlled by geology, topography and climate on the Tibetan Plateau The studied rock glacier is conceptually interpreted as the endmember of a glacier—debris‐covered glacier—rock glacier continuu

    The Minzu Debate: Policy Subsystem, Knowledge Community, and Academic Discourse in Post-Mao China’s Ethnic Policy-Making

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    How do intellectual innovations in policy fields occur under authoritarian China? In this study, I answer this question through a political-sociological investigation of the academic policy debates of the People’s Republic of China about its ethnic minority policy (a.k.a. “minzu policy”) in the Post-Mao period. Building off existing literature, I propose a theory of academic policy debates. This theory is predicated upon the political-institutional context of a policy subsystem and the internal dynamics of the knowledge community. My central argument can be summarized as follows: academic policy debates in Post-Mao China vary along two dimensions – the level of academic politicization and the theoretical heterogeneity; consequently, a debate on a given topic is a function of a) the level of conflict within the policy subsystem and b) the level of fragmentation within the knowledge community. To demonstrate this theory, I trace the changes in the conflict of policy subsystem, the fragmentation in the knowledge community, and the character of academic policy debates regarding China’s ethnic minority policy from 1979 to 2017. As I show, during this period, academic debates about minzu policy went from moderate-to-intense debate within the minzu studies paradigm to a heightened inter-paradigm debate – as the conflict among policy elites and fragmentation within the knowledge community increased – only to become somewhat moderated following the direct intervention of the party leadership to unify policy discourse. This study makes three main contributions: 1) it offers the first systematic study of the dynamics in academic knowledge production behind China’s multiethnic governance since 1979; 2) it provides a political-sociological account of the academic policy debates in Post-Mao based on a diachronic analysis of the minzu debate, thus advancing our theoretical knowledge about the political-sociological conditions for intellectual innovations in contemporary PRC’s policy field; and finally, 3) it suggests insights for understanding intellectual innovations in policy fields under authoritarian regimes more broadly
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