Educator Kim Young and Researcher Christina Minions from the Winter Respiration in the Arctic Team discuss permafrost in Alaska and what climate factors are affecting it. This presentation was broadcast live from Weston, Massachusetts on 8 April 2019.
This resource is a 2-minute immersive video that takes students inside the Permafrost Research Tunnel outside of Fairbanks, Alaska. It includes footage of both the new and old sections of the tunnel.
Objectives
Through watching this video, students will get to see what permafrost looks like from the inside, identifying typical features geological features (ex. ice wedges). Through the
This lesson plan transports students to two field sites outside of Fairbanks, Alaska to investigate the interconnected relationships between climate change and permafrost. Students will use authentic field data from site photographs, soil temperature, and thaw depth measurements to draw inferences. An ESRI StoryMap, faux field journal, and 360 site images are used to engage students in the inquiry
PolarTREC is a teacher professional development program funded through the Arctic Research Consortium of the United States (ARCUS) and National Science Foundation (NSF). PolarTREC pairs middle and high school teachers with scientific research teams to allow them to “study-abroad” as a scientific team member authentically integrated into polar (Arctic or Antarctic) field science. The PolarTREC experience facilitates
This lesson/project/lab has students predict via multiple drawings and time lapse photography predictive Flubber flow before the placement of barriers and other obstacles in front of the Flubber. Contour lines in two directions are drawn on both the paper prediction and the Flubber for comparison purposes.
Following predictive drawing completion glacier flow (Flubber flow), with obstacles in place
Ground penetrating radar is an important tool for studying glacier dynamics. Glacier scientists use GPR images to analyze attributes of glaciers. The following research activity will familiarize students with the basics of the different types of glaciers and their dynamics along with ground penetrating radar and its use in glacier studies.
Exploration of the Antarctic continent did not occur until the late 1800’s, and the South Pole was first reached on December 14, 1911. Courage, planning, and technology have been the main components of Antarctic exploration from the earliest days. This classroom activity is designed to highlight the historical elements of the past 100 years of exploration in Antarctica and
Skidompha Public Library's Chats with Champions speaker program hosted well-known Nobleboro Central School teacher Ken Williams and his former student Seth Campbell at the library's Porter Meeting Hall at 2 PM on Saturday, January 11, 2014.
The two explained the unofficial title of their presentation: "Student finally hands in 1989 homework assignment to Nobleboro teacher at 14,000 feet in Denali
Antarctica is the coldest, driest place on Earth with a fairly limited number of native species which have adapted to these extreme conditions over millions of years. As a result, it's not very likely that a non-native species would survive there . . . right? Actually ever since exploration and exploitation of the Antarctic region began in the 1800's
This story in Discover magazine profiles the work of the WISSARD (Whillans Ice Stream Subglacial Access Research Drilling) project team and the challenges faced by drilling thousands of feet into the West Antarctic Ice Sheet to reach a lake buried for millennia.