Helen Amanda Fricker | |
---|---|
Born | May 3, 1969 |
Nationality | British |
Alma mater | Bsc University College London PhD University of Tasmania |
Spouse | Glyn Fricker |
Awards | Muse Prize (2010) Fellow of the American Geophysical Union (2017) |
Scientific career | |
Fields | Glaciology Oceanography |
Institutions | Scripps Institution of Oceanography |
Thesis | Applications of ERS Satellite Altimetry in Lambert-Amery System, Antarctica (1999) |
Website | scrippsscholars |
Helen Amanda Fricker (born 1969) is a glaciologist and professor at Scripps Institution of Oceanography at the University of California, San Diego where she is a director of the Scripps Polar Center. She won the 2010 Martha T. Muse Prize for Science and Policy in Antarctica.
Helen attended Altrincham Grammar School for Girls, where she encountered Melissa Lord, a brilliant and passionate female physics teacher who steered her onto the path of becoming a scientist. [1]
In 1991, she received her B.Sc. in Mathematics and Physics from University College London (UCL), with first-class honours. [2] In her final year at UCL, she took an Earth science course from a lecturer, Chris Rapley, who was leader of the Remote Sensing Group at UCL and would later become the director of the British Antarctic Survey. Chris Rapley, encouraged her to do a dissertation on using remote-sensing data to track icebergs in the Antarctic during her final year. This course turned her attention toward Antarctica — and got her started on a career in glaciology. [3]
She earned her Ph.D. in glaciology from the Institute of Antarctic and Southern Ocean Studies, University of Tasmania, Australia in 1998. In 1999, Fricker began her work at the Scripps Institution of Oceanography as a postgraduate researcher. Fricker is now a Professor of Geophysics in the Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics at Scripps Institution of Oceanography at UC San Diego. [4] She and her husband Glyn Fricker have three daughters.
Fricker has authored over 130 publications relating to the satellite remote sensing of Antarctica's ice shelves and active subglacial lakes. [5] Fricker is widely recognized for her discovery of active subglacial lakes using ICESat laser altimetry, [6] and she has shown that these lakes form dynamic hydrologic systems, where one lake can drain into another in a short period of time. [1] Fricker was the first to describe Lake Whillans in 2007, an active subglacial lake in West Antarctica, which was subsequently the first such environment to be sampled and found to contain life. [7]
She is also known for her innovative research into Antarctic ice shelf mass budget processes such as iceberg calving and basal melting and freezing. [2] Her research focuses on ice sheets in Antarctica and Greenland and their role in the climate system and on subglacial hydrology. She uses a combination of satellite radar and laser altimetry and other remote-sensing data to understand ice sheet processes. [8] Some specific processes Fricker investigates include subglacial hydrology by monitoring the activity of subglacial lakes under the ice streams, ice flexure from tidal activity in the grounding zone, basal melting and freezing under the ice shelves, and the propagation and evolution of active ice shelf rifts, which eventually lead to iceberg calving. [8]
Fricker was one of the primary investigators on the Whillans Ice Stream Subglacial Access Research Drilling (WISSARD) project, [9] which became the first group to drill into an Antarctic subglacial lake, Subglacial Lake Whillans, in 2013 [7] [10] [11] Fricker has held numerous positions relating to her study of the cryosphere, including Chair of AGU's Cryospheric Sciences Focus Group from 2004–2006, Elected Member of the NASA ICESat Science Team from 2006–present, as part of the Ice, Cloud and land Elevation (ICESat) mission from 1999–present and the ICESat-2 Science Definition Team and the NASA Sea Level Change Team. She has been Science Team lead for ICESat-2 since May 2023. She co-chairs the Scripps Polar Center at Scripps Institution of Oceanography along with Fiamma Straneo. [12]
The Fricker Ice Piedmont was named after her by the British Antarctic Place-names Committee in 2020. [13]
Fricker received the Royal Tasmania Society Doctoral Award for her PhD in 2001. [14] She received the NASA Group Achievement Award for her role in the Ice, Cloud, and Land Elevation Satellite (ICESat) Mission Development Team in 2004. [15] In 2010, she was awarded the Martha T. Muse Prize for Science and Policy in Antarctica by the Tinker Foundation and the Scientific Committee on Antarctic Research [16] [17] She was elected Fellow of the American Geophysical Union in 2017. [18]
Lake Vostok is the largest of Antarctica's 675 known subglacial lakes. Lake Vostok is located at the southern Pole of Cold, beneath Russia's Vostok Station under the surface of the central East Antarctic Ice Sheet, which is at 3,488 m (11,444 ft) above mean sea level. The surface of this fresh water lake is approximately 4,000 m (13,100 ft) under the surface of the ice, which places it at approximately 500 m (1,600 ft) below sea level.
An iceberg is a piece of freshwater ice more than 15 meters long that has broken off a glacier or an ice shelf and is floating freely in open water. Smaller chunks of floating glacially derived ice are called "growlers" or "bergy bits". Much of an iceberg is below the water's surface, which led to the expression "tip of the iceberg" to illustrate a small part of a larger unseen issue. Icebergs are considered a serious maritime hazard.
The Byrd Polar and Climate Research Center (BPCRC) is a polar, alpine, and climate research center at Ohio State University founded in 1960.
A subglacial lake is a lake that is found under a glacier, typically beneath an ice cap or ice sheet. Subglacial lakes form at the boundary between ice and the underlying bedrock, where liquid water can exist above the lower melting point of ice under high pressure. Over time, the overlying ice gradually melts at a rate of a few millimeters per year. Meltwater flows from regions of high to low hydraulic pressure under the ice and pools, creating a body of liquid water that can be isolated from the external environment for millions of years.
Thwaites Glacier is an unusually broad and vast Antarctic glacier located east of Mount Murphy, on the Walgreen Coast of Marie Byrd Land. It was initially sighted by polar researchers in 1940, mapped in 1959–1966 and officially named in 1967, after the late American glaciologist Fredrik T. Thwaites. The glacier flows into Pine Island Bay, part of the Amundsen Sea, at surface speeds which exceed 2 kilometres (1.2 mi) per year near its grounding line. Its fastest-flowing grounded ice is centered between 50 and 100 kilometres east of Mount Murphy. Like many other parts of the cryosphere, it has been adversely affected by climate change, and provides one of the more notable examples of the retreat of glaciers since 1850.
Whillans Ice Stream is a glaciological feature of the West Antarctic Ice Sheet, formerly known as Ice Stream B, renamed in 2001 in honor of Ohio State University glaciologist Ian Whillans.
Christopher Graham Rapley is a British scientist and scientific administrator. He is Professor of Climate Science at University College London, a member of the Academia Europaea, Chair of the European Science Foundation's European Space Sciences Committee, Patron of the Surrey Climate Commission, a member of the scientific advisory board of Scientists Warning, a member of the UK Clean Growth Fund Advisory Board, and a member of the UK Parliamentary and Scientific Committee. His previous posts include Director of the Science Museum, London, Director of the British Antarctic Survey, Chairman of the London Climate Change Partnership, President of the Scientific Committee on Antarctic Research, Vice President of the European Science Foundation's European Polar Board, Executive Director of the International Geosphere-Biosphere Programme, and founder and leader of UCL Mullard Space Science Laboratory's (MSSL) Remote Sensing Group.
There are hundreds of antarctic lakes in Antarctica. In 2018 researchers at the Alfred Wegener Institute for Polar and Marine Research published a study they claimed cast doubt on the earlier estimate that there were almost 400 subglacial antarctic lakes. Antarctica also has some relatively small regions that are clear of ice and snow, and there are some surface lakes in these regions. They called for on the ground seismic studies, or drilling, to determine a more reliable number.
Lake Whillans is a subglacial lake in Antarctica. The lake is located under the Whillans Ice Stream at the southeastern edge of the Ross Ice Shelf in the west of the continent. The lake surface is 800 m (2,600 ft) beneath the surface of the ice and the lake covers an estimated area of 60 km2 (20 sq mi). Lake depths measured thus far have been around 2 metres. Its temperature is −0.49 °C, below 0 °C because of the high pressure.
Lake CECs is a subglacial lake in Antarctica at approximately latitude 80°S. It has an estimated area of 18 km2. The territory where the lake is located, some 160 km from Union Glacier, is claimed only by Chile.
Jemma L. Wadham is a British glacial biogeochemist.
Liu Yan is a Chinese Antarctic researcher best known for her work on iceberg calving. She is an associate professor of geography in the College of Global Change and Earth System Science (GCESS) and Polar Research Institute, Beijing Normal University.
Trista Vick-Majors is an American Assistant Professor in Biological Sciences at Michigan Tech. She is an Antarctic biogeochemist and microbial ecologist, best known for her work showing that microorganisms are present under the Antarctic ice sheet.
Burcu Özsoy is a Turkish scientist who works with sea ice remote sensing in Antarctica. Özsoy is head of the first Turkish polar research center, ITU PolReC.
Martin J. Siegert is a British glaciologist, and Deputy Vice Chancellor (Cornwall) at the University of Exeter. He co-Chairs the Diversity in Polar Science Initiative, and has spoken about socio-economic inclusion in Polar Science and indeed broader society.
Sophie Marie Jeanne Nowicki, is Empire Innovation Professor in the Department of Geology of the University at Buffalo. She does research on the Greenland and Antarctic ice sheets, focusing on their connections to global climate and sea level. Before that, she was physical scientist at the Nasa Goddard Space Flight Centre, investigating ice sheet changes.
Mercer Subglacial Lake is a subglacial lake in Antarctica covered by a sheet of ice 1,067 m (3,501 ft) thick; the water below is hydraulically active, with water replacement times on the order of a decade from the Ross Sea. Studies suggest that Mercer Subglacial Lake as well as other subglacial lakes appear to be linked, with drainage events in one reservoir causing filling and follow-on drainage in adjacent lakes.
Salty subglacial lakes are controversially inferred from radar measurements to exist below the South Polar Layered Deposits (SPLD) in Ultimi Scopuli of Mars' southern ice cap. The idea of subglacial lakes due to basal melting at the polar ice caps on Mars was first hypothesized in the 1980s. For liquid water to persist below the SPLD, researchers propose that perchlorate is dissolved in the water, which lowers the freezing temperature, but other explanations such as saline ice or hydrous minerals have been offered. Challenges for explaining sufficiently warm conditions for liquid water to exist below the southern ice cap include low amounts of geothermal heating from the subsurface and overlying pressure from the ice. As a result, it is disputed whether radar detections of bright reflectors were instead caused by other materials such as saline ice or deposits of minerals such as clays. While lakes with salt concentrations 20 times that of the ocean pose challenges for life, potential subglacial lakes on Mars are of high interest for astrobiology because microbial ecosystems have been found in deep subglacial lakes on Earth, such as in Lake Whillans in Antarctica below 800 m of ice.
Sinéad Louise Farrell is a British-American space scientist who is Professor of Geographic Sciences at the University of Maryland, College Park. Her research considers remote sensing and climate monitoring. She was science lead for the ICESat-2 Mission, which used laser altimetry to make height maps of Earth.
Catherine Walker is an American Earth and planetary scientist at the Woods Hole Oceanographic Institution, where she is on the scientific staff in the Department of Applied Ocean Physics and Engineering. Her research spans fracture mechanics and dynamics in ice, cryosphere change, physical oceanography, and geomorphology on Earth and other planets and moons using a variety of methodologies including remote sensing.