The long-term objective of PolarTREC teacher Lesley Urasky's expedition research in Antarctica (Glacial History in Antarctica) is to determine the rate at which glaciers have receded since the Last Glacial Maximum. This lesson is designed to give students an understanding of the Last Glacial Maximum, the climatic conditions that lead to glacial periods, and how the rate of glacial
PolarTREC teacher Nell Herrmann writes a compelling article for Town and Gown, the local newspaper in her home town of State College, PA. Nell reports on her adventures with a team of scientists in Antarctica and the profound way in which her journey has influenced her both personally and professionally. Note: The online article starts on p. 50 of the
Listen in to this radio interview on National Public Radio's program, "All Things Considered" with PolarTREC teacher Nell Herrmann. Nell describes her excitement about traveling to Antarctica and her role in a study of Antarctic seafloor organisms and their response to changes in water acidification and temperature. Nell outlines her plans for sharing the research team's findings with her students
"It is so much more meaningful to students to have real world applications of science. It helps them make connections and broadens their understanding of science"
This article highlights Nell's upcoming PolarTREC field expedition to Antarctica as well as the many educational excursions she has undertaken around the world that have influenced her teaching and her life.
Article about PolarTREC teacher Nell Herrmann's expedition to Antarctica written by her former student. The article was published in The Lion's Digest, her school's newspaper in State College, Pennsylvania.
Even in Antarctica ice will melt. As the sun stays higher and higher in the sky as summer progresses, the warm sun causes the ice to melt. The questions that we are going to ask are: 1) Does clean ice (no sediment) or dirty ice (has sediment mixed in it) melt faster? and 2) Would the ice melt if
For this experiment, we are going to melt dirty ice (ice with lots of sediment/dirt in it) and clean ice (ice without sediment) from the Taylor Glacier. After we melt the ice, we are going to test the melt water for pH and conductivity, and then determine how much salt is actually in our ice samples. There are
This data plotting lesson compares different stratospheric ozone data collected at the South Pole in September 1969, September 1998, September 2008, January 1999, and January 2008. This ozone comparison activity allows students to make conclusions about the annual and seasonal ozone hole as well as overall ozone concentration changes over Antarctica. Students use authentic data collected at the