The Svalbard REU: Holocene and Modern Climate Change in the High Arctic

Since 2003, the Principal Investigators have been administering a summer REU site on the Svalbard archipelago for motivated geoscience undergraduate students. The students undertake important climate change research and experience the challenges and rewards of conducting high latitude research. The...

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Bibliographic Details
Main Author: Steven Roof
Format: Dataset
Language:unknown
Published: Arctic Data Center 2012
Subjects:
Reu
Online Access:https://search.dataone.org/view/urn:uuid:1b96e994-20a1-4445-a327-3256c040034f
Description
Summary:Since 2003, the Principal Investigators have been administering a summer REU site on the Svalbard archipelago for motivated geoscience undergraduate students. The students undertake important climate change research and experience the challenges and rewards of conducting high latitude research. The primary research goal is to understand how climate influences the modern glacial, fluvial lacustrine, and fjord systems. By studying these modern processes, students will interpret the sediment record as a high-resolution record of late Holocene climate change. The students are integrally involved in defining their research questions and designing specific testable hypotheses throughout the program. They complete their research projects at their home institutions during the following academic year. This project collaborates closely with UNIS, the University Centre onSvalbard, with both UNIS students and faculty working together during the summer field season. Intellectual Merit: The Arctic is an area of active research because it is highly sensitive to climate change and because climatically induced environmental changes in this region can instigate further changes of global consequence. Recently published data indicate that the Arctic is warming much faster than lower latitudes and even greater rates of change and ecosystem disruption are predicted with the continuing decay of the Arctic Ocean pack ice. Svalbard is strongly influenced by the northern end of the warm Gulf Stream current, and therefore its climate is sensitive to changes in global scale oceanic circulation. Svalbard has warmed considerably during the last 90 years and climate proxies indicate even greater Holocene climate variability. Despite this, little is known of sub-century climate change and virtually nothing is known of decadal scale variability in this Arctic region. This project has initiated long term monitoring of the rapidly changing Arctic cryospheric/hydrosphere that will facilitate interpretation of high-resolution proxy records from the Svalbard region. Broader Impacts: This project benefits society by recruiting and training the next generation of Arctic researchers, and our modern process studies will directly improve predictive models of future climate change by strengthening the link between climate processes and climate proxies. We make every effort to recruit students from diverse populations and from institutions lacking in-house research opportunities. The Principal Investigators, undergraduate participants, and participating K-12 teachers make frequent and wide-reaching outreach to public audiences on Arctic climate change issues and the importance of science education, increasing awareness of Arctic environmental change in K-12 classrooms around the world. Funding Source: Arctic Natural Sciences (ANS) Sponsor: Hampshire College, 893 West Street, Amherst, MA 01002-3372 Related URLs: - Mount Holyoke College Svalbard - REU Project Page: https://www.mtholyoke.edu/proj/svalbard/welcome.shtml - Mount Holyoke College Svalbard - REU Data Access Page: https://ida.mtholyoke.edu/jspui/handle/10166/2