My PolarTREC expedition to the Dry Valleys of Antarctica was an experience of a lifetime. Notice I did not use the word “trip” of a lifetime. This was far more than a trip. It was an experience that is a life-changer. It has been a life-changer for myself, my students, my family, other educators, and other folks
PolarConnect Event with Kevin Dickerson and Dr. Byron Adams discussing the science and field work taking place for the Dry Valleys Ecosystem Study in Antarctica. This event took place on 6 February 2019.
In this investigation, students will measure production of CO2 from surface water and consider the role of surface waters in the global carbon cycle and climate change. They will gather data on using Vernier CO2 sensors. This lesson presents a wonderful opportunity for student-designed experiments.
This is a good lesson to get students thinking about the complexity of the systems involved in providing our society with energy, the consequences of energy use and efficiency. Students are encouraged to explore the data sets on their own, ask their own questions about energy use and present their findings to each other.
This outreach piece in Nature describes the aspects of bringing various guests on field science expeditions. The PolarTREC program is a focus amongst the programs providing some best practices as the author offers advice to scientists considering the addition of guests on expeditions.
This article and associated video describe the findings of researchers who undertook core drilling at Lake El’gygytgyn, a lake that sits today inside a basin formed by a meteorite that struck the earth 3.6 million years ago. An associated video allows us to hear the enthusiasm and details as researcher Julie Brigham-Grette describes the findings of this remarkable discovery.
This article describes the remarkable efforts of a team of scientists to extract cores from deep under a frozen lake in Siberia, Russia. PolarTREC teacher Tim Martin joined the project which will provide an astounding record of past climates preserved in layers of lake bed sediment. The sediment, withdrawn in cores and shipped to labs in Germany, represents a continuous