I met up with the team of researchers from the US Geological Survey who had been performing polar bear captures out of Barrow already for two weeks. That evening, after looking over our gear and getting caught up, I went over to see friends who recently moved to Barrow from Wyoming. It was great to hear about their new life in the area; moving from the mountains to the tundra is certainly a big change.

The next day I began flying in the helicopter for captures. We started in Barrow, fueled up in Deadhorse, and ended the day in Kaktovik, near the Canadian border – we covered almost the entire northern coast of Alaska. Since then we have been based out of Kaktovik, and we have had good weather and have been flying a lot.

It is great to be back out on the sea ice. Although I am out of place here, I really love this environment. In this picture we landed on a small pan of ice about twenty miles from shore; the pan was surrounded by pressure ridges and rubble from ice sheets smashing into each other.

The captures have been going well. We caught the largest bear I have seen, an adult male who weighed 1,147 lbs (I am not sure what the largest bear caught in the southern Beaufort has weighed). His neck was several times the size of my waist, and I could not fit both hands around his snout. It took several people to position him for measurements. We have caught several bears which were sampled in 2009, giving us excellent data on changes over time in the same individual.

We have also caught a lot of cubs-of-the-year, or COYs, including this litter of three. Cubs are born around January 1st. Litters of three are fairly uncommon for polar bears in Alaska, and usually include one cub that is noticeably smaller than the others – in this picture, the cub in the middle only weighed 12 lbs, nearly 10 lbs less than the other two.

This short video sums up pressure ridges. The pressure ridges we explored here form where a large mass of sea ice buckles under pressure as it makes contact with land (in this case, Ross Island where McMurdo Station and Scott Base are located). The wind, tides, and sun are all variables that constantly change these ridges. With Mt. Erebus looming over the station, the views were quite dramatic. Surprisingly, every view along our ~2 mile walk seemed different! It was like walking through a park of ice sculptures! Like identifying shapes in clouds, we were able to see a dog, person, peace sign, and set of waves. I hope you enjoy this short video with photos from this little adventure onto the ice!

Music by Wayne Grim.

The Christchurch Botanic Gardens, New Zealand.

The Croquet Club, Christchurch.

On Dec 9 we were scheduled to take a South African Hercules to McMurdo but ended up flying on the massive C17 “Globemaster” instead. The C17 was going to make an aidrop to “AGAP” after it dropped us off in McMurdo. You can see that the air-drop cargo was all ready to go (there is a parachute on top of each piece of cargo).

The C-17 ready for Airdrop.

During the flight I saw a lot of pack ice, and also got a nice photograph of the Antarctic coastline. We landed at Willy field (a runway on the sea ice). It was a nice day and you could see Mount Erebus in the distance (an active volcano).

Pack ice from the air.

The Antarctic coastline.

The C-17 ‘Globemaster.’

After being debriefed and getting our room assignments I took the Terrabus over to Scott Base (the New Zealand station). From there I could see the pressure ridges, and also the Happy Camper (Antarctic survival training) folks in the distance.

Having landed at McMurdo Station with Mt. Erebus in the background.

Scott Base pressure ridges, Terrabus and Happy Camper at foot of Mt. Erebus.

I knew that Mary Miller and Lisa Strong from the Exploratorium were standing there next to the two Scott Tents. The Happy Camper school was taking place at the foot of Mount Erebus. In the photo above, you can see the Terrabus between the pressure ridges and the Happy Camper school.

Because being at high altitude can make some people sick, the science team has to be trained on multiple parts of the airplane’s science equipment.

During June this year, we tested our radar system in Greenland. We flew over the Greenland Ice Sheet, collecting data to image the ice down to 2.5 km (1.6 miles) below the lake-spotted surface. Now in Antarctica, we face the challenge of imaging more than 4 km of ice…. That’s 2.5 miles of frozen history between our science team and the Gamburtsev Mountains we came here to study! Because we have to reach further into the ice, we have more data than ever coming back after each flight. There’s so much data that the system chokes on it and gasps, “Help me, Adrienne. Help!”

I have escaped the office a few times this week. I got to go on a tour of the pressure ridges that form between the flowing ice of the Ross Ice Shelf and the rock that stands firm against it. And just last night, I escaped to Scott Base, the Antarctic Base that belongs to New Zealand, for some retail therapy. My Scott Excursion really took my mind off of the software for a while and had me refreshed and ready to go back to Radar World this morning. Not to mention I am well stocked on wooly base layers to fight the cold.

View of Scott Base from the Pressure Ridges.

An interesting formation in the Pressure Ridges. What do you think it looks like?

Today, I feel the same way I do when I am at the top of the big hill at the beginning of the ride. There’s that moment when you lift off your seat before powering down the steep hill, screaming your head off. I have been living there, in that emotional suspension for 3 days. Part of my jitteriness the last few days is undoubtedly rooted in the fact I’ll be going to the South Pole on Monday. According to our medical briefing, that means I’ll be perpetually short of breath, having trouble sleeping and going to the bathroom about every 20 minutes for 2 days…. The anticipation is almost too much to hold in! I have been to 10,000ft elevation before but that was after living at 6,500ft above sea level for 5 weeks… and that was in Utah. The transition from sea level here in McMurdo to 10,000ft is such a surprise to the system that everyone is prescribed a medication to help our bodies adjust to the lower oxygen levels. On top of that, we all have to fight off the adrenaline brought on by the fact we’re in Antarctica, at The South Pole, at 10,000ft—no offense to Utah, but it doesn’t compare! Just in case we don’t adjust to the elevation, everyone has been learning tasks outside their specialty. Hopefully, if someone gets sick, we’ll be able to keep the science moving forward, even if at a slower pace.

In the end, it’s not just where we’ll be a week from now. It’s what we’ll learn. The Gamburtsev Mountains have been enigmatic since their happenstance discovery in 1958. Soon, we’ll know them in a way only dreamt of until now. The people on this science team will learn more about the Mountains than the rest of the world has compiled in the last 50 years. This is the Eve of Discovery.