My name's Dave Eastmont.
I'm the mission manager for Wallops aircraft at this time. My previous experience
has been with the P-3. I've done DC-8 flights I've done Aerosonde UAV flights.
and C-130 flights. I've probably got upwards to about
4,000 hours in the back of the plane.
My name's Bill Krabill. I'm the project scientist
for Operation Ice Bridge. And I've been flying missions
like this to Greenland since 1991.
The aircraft behind me is NASA's P-3
research aircraft. It's used as a platform
for various remote sensors. And we're going to be using it
in Greenland this year, as we have most years since 1991
to collect a suite of measurements to tell the scientists
the thickness of the ice and how fast it's flowing
out to the ocean. And what we're observing is
the decade of the '90s was exhibiting very
small changes. If we saw a half a meter to a meter
per year of thinning, that was a pretty large number in that time
frame. But since the turn of the century, we're seeing
the same glaciers now thinning at 15, and 20, and 25 meters
per year. So there's some very drastic changes taking place up in Greenland.
The additional work that we'll be doing
for Operation Ice Bridge will be to follow the exact
orbit paths on the surface that ICESat has followed
in the past and will follow in the future and that ICESat II would follow
when it gets launched in 2015.
It does a very nice job of global coverage
particularly of Antarctica that's quite remote and very difficult to get to with
an airplane. So whereas the typical flights that we would
make in the past are focused, targeted towards the outlet
glaciers, we'll now also do the same kinds of measurements
that a satellite would, and this sort of ties the two projects together.
I'm Jim Yungle,
I'm a lead engineer on the NASA Airborne Topographic Mapper Project.
It measures the elevation of the terrain the aircraft flies over
by firing pulses of laser light from the aircraft to the ground
and back. Those pulses are scanned in an oval scan
and this allows us to map a swath of terrain
underneath the aircraft, and it allows us to return in a future
year and repeat those measurements pretty accurately.
We're concerned with the icesheets of the world
because to some degree they control sea level.
Greenland is the second-largest ice sheet in the world. It contains enough
ice and snow that if it were to melt it would raise sea levels
substantially, maybe as much as 20 feet in this area. You can imagine Greenland
as a huge ice cube that's a thousand miles long and
400 miles wide and two miles thick in the center.
It buffers global climate, regional climate so
that changes in the ice sheet become very important
indicators of global climate change.
It's something you have to experience ...
we'll fly these patterns at 1,500 feet,
above the ground level. And you get up on the ice sheet it's like flying over the clouds.
And you look down and it's white, fluffy sometimes -- it just looks like a cloud.
You have to keep in your head that it's solid underneath you.
Probably one of the neatest things to see is when you're flying
down the glacier toward the ocean, you're at 1,500 feet and just as you hit the ocean
the glacier drops off another thousand feet. No matter now
often you do it, it always takes your breath.