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Byrd Polar and Climate Research Center
The Byrd Polar and Climate Research Center (BPCRC), formerly Institute for Polar Studies, is a polar, alpine, and climate research center at Ohio State University founded in 1960.
The Byrd Polar Research Center (BPRC) at Ohio State University was established in 1960 as the Institute for Polar Studies. BPRC is the oldest research center at Ohio State University. The name was changed to the Byrd Polar Research Center in 1987 after the polar explorer and aviator Richard E. Byrd when Ohio State purchased the Byrd papers from the Byrd family in 1985.
BPRC conducts interdisciplinary research at the nexus of Earth Sciences and Engineering. BPRC is known for its ice core paleoclimatology research collecting ice core records from Earth's highest and most remote ice fields and modeling polar climate variability. Studies at BPRC include paleoclimatology, remote sensing, polar meteorology, glacier dynamics, satellite hydrology, paleoceanography, environmental geochemistry, and climate change. BPRC houses the Polar Rock Repository and the Goldthwait Polar Library.
The Environmental Geochemistry group collects and analyzes soil and water samples from many locations around the world to study biogeochemical cycles, anthropogenic influences on natural systems, and to use geochemistry as a tool to learn more about various hydrological, biological and physical processes.
This group has conducted studies of the Dry Valleys region of Antarctica since 1993 as part of the NSF’s Long-Term Ecological Research (LTER) program. Ongoing projects in Antarctica include drilling into the subglacial ecosystem of "Blood Falls" in the Dry Valleys and measuring glacial melt input into the Southern Ocean in West Antarctica. Additionally, the group has studied of the deposition of mercury on the landscape in the U.S. and in Antarctica, and led investigations of chemical and physical weathering of rocks of high-standing oceanic islands like Taiwan and New Zealand. Members of this group also study the impact of human activities in urban areas on streams and lakes around Ohio.
The Paleoceanography group uses information gathered from sea floor sediments to discover how changes in circulation, temperature, sea ice and glacier mass have affected the global climate system throughout Earth’s history. These data from the past are used to assess present and future climate changes. The main focus of this group's research is on the Arctic Ocean and its history during the past several million years.
Sea floor sediments contain mineral and biological particles that are used for investigating past climate changes. A common type of biological particles is foraminifers, single-celled, amoeba-like protists that have a shell and either live on the sea bottom or float in the upper water column. There are an estimated 4,000 species living today. Foraminifers are sensitive to changes in their environment such as temperature and salinity, which makes them useful indicators (proxies) of past climate changes.
This group uses satellite-based measurements to study rivers, lakes, wetlands, and floodplains. Led by Profs. Douglas Alsdorf and Michael Durand, group members primarily use passive and active microwave measurements such as radar to measure surface water and snowpack. This group is working to better quantify the amount of water stored in snowpacks in the United States using satellite measurements.
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Byrd Polar and Climate Research Center
The Byrd Polar and Climate Research Center (BPCRC), formerly Institute for Polar Studies, is a polar, alpine, and climate research center at Ohio State University founded in 1960.
The Byrd Polar Research Center (BPRC) at Ohio State University was established in 1960 as the Institute for Polar Studies. BPRC is the oldest research center at Ohio State University. The name was changed to the Byrd Polar Research Center in 1987 after the polar explorer and aviator Richard E. Byrd when Ohio State purchased the Byrd papers from the Byrd family in 1985.
BPRC conducts interdisciplinary research at the nexus of Earth Sciences and Engineering. BPRC is known for its ice core paleoclimatology research collecting ice core records from Earth's highest and most remote ice fields and modeling polar climate variability. Studies at BPRC include paleoclimatology, remote sensing, polar meteorology, glacier dynamics, satellite hydrology, paleoceanography, environmental geochemistry, and climate change. BPRC houses the Polar Rock Repository and the Goldthwait Polar Library.
The Environmental Geochemistry group collects and analyzes soil and water samples from many locations around the world to study biogeochemical cycles, anthropogenic influences on natural systems, and to use geochemistry as a tool to learn more about various hydrological, biological and physical processes.
This group has conducted studies of the Dry Valleys region of Antarctica since 1993 as part of the NSF’s Long-Term Ecological Research (LTER) program. Ongoing projects in Antarctica include drilling into the subglacial ecosystem of "Blood Falls" in the Dry Valleys and measuring glacial melt input into the Southern Ocean in West Antarctica. Additionally, the group has studied of the deposition of mercury on the landscape in the U.S. and in Antarctica, and led investigations of chemical and physical weathering of rocks of high-standing oceanic islands like Taiwan and New Zealand. Members of this group also study the impact of human activities in urban areas on streams and lakes around Ohio.
The Paleoceanography group uses information gathered from sea floor sediments to discover how changes in circulation, temperature, sea ice and glacier mass have affected the global climate system throughout Earth’s history. These data from the past are used to assess present and future climate changes. The main focus of this group's research is on the Arctic Ocean and its history during the past several million years.
Sea floor sediments contain mineral and biological particles that are used for investigating past climate changes. A common type of biological particles is foraminifers, single-celled, amoeba-like protists that have a shell and either live on the sea bottom or float in the upper water column. There are an estimated 4,000 species living today. Foraminifers are sensitive to changes in their environment such as temperature and salinity, which makes them useful indicators (proxies) of past climate changes.
This group uses satellite-based measurements to study rivers, lakes, wetlands, and floodplains. Led by Profs. Douglas Alsdorf and Michael Durand, group members primarily use passive and active microwave measurements such as radar to measure surface water and snowpack. This group is working to better quantify the amount of water stored in snowpacks in the United States using satellite measurements.
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