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How do you get under an ice
layer two meters thick (six feet) to go scuba diving?Use a big drill !
A work crew drives out in tracked vehicles to a prospective dive site near
McMurdo Station. The crew uses a large auger mounted on the back of a tracked
vehicle to bore holes through the ice

These holes will be used by scuba divers from McMurdo Station to
get under the ice.
Two holes are drilled; a secondary safety hole is drilled
a short distance away from the primary dive hole. Seawater comes up the auger
when it has drilled all the way through the six foot thick sea ice ceiling.

The
work crew sleds a dive hut out to the dive site and parks it directly over the
primary dive hole they just drilled. As shown here, snow is piled around the
hut's base to seal out the strong Antarctic wind; otherwise snow will blow into
the hut through the hole in the hut's floor. Warmed inside by a heater, the
scuba diver is protected from the elements while suiting up and getting in and
out of the water.

Here's
the primary dive hole under the dive hut. The water is near the top
of a dive hole and the diver drops down six feet through that hole of ice until
coming out under the sea ice ceiling. Obviously the diver cannot be
claustrophobic ! There is a layer of platelet ice beneath the sea ice
consisting of small ice crystals and large platelets; these are dislodged by
divers' bubbles and float into the hole as seen here. A long-handled dipnet is
used to keep the dive hole open and free of this ice.

A
weighted drop line (seen here at the left of the diver)
hangs straight down from the primary dive hole and has the following attached:
black and white checkered flags, two to three strobes, and a pony bottle (extra
emergency air) with regulator. The drop line can be used to descend to and
ascend from the bottom immediately under the dive hole if there is a strong
underwater current. The drop line is also a useful point of reference for the
diver's safety stops to prevent decompression illness. The diver sees the flags
close by and can see those strobes from far, far away. As the submerged diver
looks up, the primary dive hole is rather dark since there is a hut over it
(though still lighter in shade than the sea ice ceiling).
The
secondary dive hole is a safety hole out in the open a short distance
away from the dive hut. It is used in case the primary hole is blocked by a
Weddell seal. Topside, the safety hole is marked with a flag pole
(so the divers can find it after a blizzard) and is covered with a foam
plug when not in use (to prevent freeze-over).
When a submerged diver looks up at the sea ice ceiling, the secondary
hole has bright light streaming down on a sunny day, because it is out in the
open and not under the dive hut. This bright light shining down the hole makes
it easy for the diver to spot the dive hut and hole location from far away. It
is easy to dive safely under the ice by remaining in the vicinity of these dive holes. There was
usually only a very slow current so a diver didn't have to worry about getting
swept away from the dive hole. There was no underwater surge complicating
diver activities. Due to the ice ceiling, there were no waves affecting
dive operations at the surface. In addition, we didn't have to pay attention to
tides. Antarctic tidal movement is unique in the world's oceans because there
are no significant land masses to impede the East/West (counterclockwise) sweep
of the tides around the Antarctic continent [1]. Antarctic
tidal movement is principally a progressive wave, and the tide is diurnal (one
high water and one low water each tidal day, a lunar day of 24 hours and 50
minutes) [1].

If it is very cold, particularly in a strong wind as shown
here, an ice crust slowly forms over the outside secondary dive hole. This
crust has to be removed so that submerged divers can exit through this outside
hole in an emergency. The ice crust is broken up with a pole or chipper bar
(in the diver's hands) and then pieces are fished out
with a dipnet (behind the diver).

Diving under the ice from a dive hut is comparative luxury
compared to diving out in the open. At locations far away from McMurdo Station,
a hut may be unavailable (like Discovery Bluff at Granite Harbor
as shown here). Divers then enter the water through holes in sea ice
cracks, either seal-made or man-made. This hole was seal-made and was shared
with Weddell seals. Weddell seals enlarge holes in sea ice cracks for their use
and keep them open throughout the year.If seal-made holes are unavailable,
divers may open up a hole along a crack, using hand tools or chainsaws.

When diving close to McMurdo Station, a hole can be drilled in the ice (as shown above), or a Weddell seal hole can be used
(as shown here at Turtle Rock). There may be a bit of
wiggling involved to fit through restrictions in a Weddell seal hole. Here a
diver has finished a dive and has handed out his air tank. Next he will lift out
his weight harness, and then hoist himself out of the hole.
Here's
a diver's eye view looking up at a Weddell sea hole used by our team to dive. The Weddell
seals keep these holes open year round with their teeth, pivoting around in the
hole, gnawing at the ice. That's why this seal hole looks so round. If divers are polite
and ask first, the Weddell seals will let divers use these holes. Divers don't
linger in these seal holes for very long, because the seals need them to breathe
while in the water, and to get in and out of the water. One member of our dive
team was poked about his rear end as he floated in a seal hole. Another member
of our dive team waited underwater to exit, while two Weddell seals fought it
out over temporary turf rights to the hole.

Here's another diver's eye view looking up at a Weddell sea hole used to
dive on a grounded iceberg offshore Cape Barne (no dive
hut). You are looking up at the underside of a crumpled
pressure ridge of sea ice alongside that grounded iceberg. You can see the drop
line hanging down from the hole and used by the divers for a point of reference
and tie-off for emergency air supply. When there is a current, the drop line is
used for handholds while descending to the seafloor and ascending to the surface, in order to
avoid drifting away with the current.
1: Sailing Directions (Planning Guide &
Enroute) Antarctica. Publication 200. National Imagery and Mapping Agency,
Bethesda, Maryland. 1997. page 77
| Text
©Peter Brueggeman. Photographs ©Peter Brueggeman, Kevin Hoefling, & Norbert Wu.
Photographs may not be used in any form without the express written permission
of Peter Brueggeman, Kevin Hoefling, & Norbert Wu..
Norbert Wu no longer grants permission for uncompensated use of his photos under any circumstances whatsoever;
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