Titlebook: Global Change and Mountain Regions; An Overview of Curre Uli M. Huber,Harald K. M. Bugmann,Mel A. Reasoner Book 2005 Springer Science+Busin

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A Dynamical Perspective on High Altitude Paleoclimate Proxy Timeseriestional factors. In this chapter, we highlight two methods which use dynamical constraints, either from the climate system or the underlying archives themselves, to help tease out the climatic information contained in point-based proxy timeseries. Although the examples that we present are applied in

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Ice Cores from Tropical Mountain Glaciers as Archives of Climate Changeine cores, corals, etc., they provide an unprecedented view of the Earth’s climatic history over several millennia. This paper provides an overview of these unique glacier archives of past climate and environmental changes on millennial to decadal time scales. Also included is a review of the recent

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The Contribution of Cosmogenic Nuclides to Unraveling Alpine Paleoclimate Historiesrectly determines when the glacier reached a measurable mass-balance condition, whereas other chronometers, such as radiocarbon, U-series, and luminescence dating, typically provide only minimum or maximum limiting ages on ice margin positions, (ii) The method can provide a precise estimate of the t

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Holocene Environmental Change in the Himalayan-Tibetan Plateau Region: Lake Sediments and the Future longer-scale extremes in monsoon. A major goal of this paper is to summarize the state-of-the-art regarding century to millennium-scales of monsoon variability, and to identify the paleoenvironmental research that is most urgently needed in the Himalayan-Tibetan Plateau if society is to be served e

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Long-term Responses of Mountain Ecosystems to Environmental Changes: Resilience, Adjustment, and Vulof processes across both steep environmental gradients and different time scales, we may be able to better estimate ecosystem responses to current and future environmental change (Ammann et al. 1993; Lotter et al. 1997).

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https://doi.org/10.1007/978-1-4684-8160-0tional factors. In this chapter, we highlight two methods which use dynamical constraints, either from the climate system or the underlying archives themselves, to help tease out the climatic information contained in point-based proxy timeseries. Although the examples that we present are applied in

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A Critique of Polarity and Sovereignty,rectly determines when the glacier reached a measurable mass-balance condition, whereas other chronometers, such as radiocarbon, U-series, and luminescence dating, typically provide only minimum or maximum limiting ages on ice margin positions, (ii) The method can provide a precise estimate of the t

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