Lesley Anderson was connected with local California radio station KSON before and during her trip to South Pole, Antarctica as part of the PolarTREC program.
1. KSON Radio Station hosts a live interview with Lesley Anderson at the food fund in Bonita, CA.:
http://www.kson.com/media/audio-channel/john-and-tammys-food-fund-friday-bonita
2. Article in John & Tammy Blog (see downloadable article).
3. Facebook post during her stay
The Star News, a Chula Vista newspaper interviews Lesley Anderson about her experience studying neutrinos at the South Pole and her plans to bring the research back into her classroom.
Oftentimes called “ghost particles,” neutrinos can travel through nearly everything (the sun, the earth, you!) undetected. Because they are nearly massless, gravitational fields do not affect neutrinos; Similarly, because they are chargeless, electric and magnetic fields do not con affect neutrinos. This lack of interaction is advantageous for IceCube researchers – when they detect a neutrino, it is a
In this lesson, students will be introduced to the Standard Model, learning key vocabulary such as Fermions, Hadrons, Mesons, Baryons, Quarks, Leptons, particles, and anti-particles. In particular, students will come to understand what a neutrino is and why it is such a unique particle. This understanding connects to the IceCube Neutrino Observatory’s search for neutrinos in an effort to
The Dry Valleys region in Antarctica is known as the coldest, windiest, driest place on Earth. Beacon Valley is famous for its katabatic winds which can routinely knock fit adults and PolarTREC teachers to the ground. This lesson was created by PolarTREC teacher Jacquelyn Hams who experienced the cold and the full force of the winds in 2008
The Antarctic Research Group at Boston University is lead by Dr. David Marchant. Graduate students include Adam Lewis, Doug Kowalewski, and Kate Swanger.
Marchant's ongoing NSF funded research projects focus on:
1. Age, origin, and climatic significance of buried ice in the Dry Valleys region, southern Victoria Land
2. Response of the East Antarctic Ice Sheet to middle Miocene global