9 November, 1997
9 November 97
1700L SEVERE WEATHER CONDITION
Condition I for the Ice runway, ice road, Williams field, snow raod, road
to Williams field.
Condition III Mcurdo, Scott base, Road to Scott base, Arrival heights,
T-Site.
REGIONAL WEATHER SUMMARY...A low north of Marie Byrd land is spreading an
extensive area of cloud and snow across the Ross Ice shelf and into the
McMurdo area. Gusty winds will gradually diminish overnight but periods
of snow and blowing snow will continue to produce visibility reductions
at times.
TONIGHT...Cloudy with periods of light snow and blowing snow.
Visibility: 4-6 miles.
Wind (knots): Southeast 15 to 25.
Temperature steady near -05/+23F Lowest Wind-chill -26C/-15F.
MONDAY...Mostly cloudy with occasional periods of light snow. Some
blowing snow on the sea ice.
Visibility: Unrestricted occasionally 3-6 miles in blowing snow.
Wind (knots): Southeast 10-15.
Temperature steady near -05/+23F Lowest Wind-chill -26C/-15F.
SCOTT BASE 24HR TEMPERATURE FORECAST
Temperature steady near -6
ASTRONOMICAL DATA
Next sunrise in February, 1998
YESTERDAY'S EXTREMES: 08 November, 1997
Maximum Temperature: -02C/+28F
Minimum Temperature: -08C/+18 F
Peak Wind: 39 Knots
Lowest wind chill: -23C/-10F
Sunday is the one day life at McMurdo is recognizably different from any
other day. The pace of life is a little slower and people are more likely
to engage in personal activity and recreation. This was a beautiful day
and the temperature was downright balmy hanging in the mid 20's F all day
and night (which are the same thing here).
It's funny how relative the temperature is. On Scott's expedition in
1911 one party routinely hauled sledges in -70 F. degree temperatures and
looked forward to the days when it was -50F because they were so warm.
Back at my home in Buffalo I would think winter temperatures in the 40's
were downright hot spells, yet if it went into the 50's during the summer
months the cold was intolerable. Here in Antarctica if one mentally
prepares for the cold and dresses appropriately it's quite tolerable.
Nevertheless it is a real treat to experience a day of truly beautiful
weather like we had today.
I slept in and did some laundry before going to brunch at 11:00AM.
After brunch I decided to go to Scott Base, which is operated by New
Zealand, and not far away. When I returned I met Sandy Shutey who is
another teacher in this program. She has just arrived in McMurdo and is on
her way to the large field camp at Siple Dome. She will be parcticipating
in a major ice core study involving factors which affect how chemicals
interact with the polar ice sheet. You can find out more about this by
going to her web page on this site.
The Cape Roberts Drilling Project had an open house today in their Crary
Lab facility. I discussed this project in my journal entry of 28 October
and detailed how the big storm of 23 October (see journal entry for 23
October) caused this international project to be shut down. The scientists
involved with the project put together a wonderful open house for the
McMurdo community. They gave tours, explained their research, had
demonstrations and hands-on opportunities to look at microfossils recovered
from the cores, and even had sections of the cores on display. I returned
to the lab to catch up on some odds and ends then headed to the galley for
dinner.
It is customary to have a lecture after Sunday dinner. This week's
lecture was by Dr. Peter Barrett who is the scientist that heads the Cape
Roberts Project. His talk described the historical development of the
project and its scientific goals. As mentioned in other entrys, more than
50 scientists from 28 institutions representing 6 countries are involved in
this undertaking.
These scientists had their drill rig set up on the seasonal ice near
Cape Roberts. They drilled through the ocean floor and hoped to recover
core samples from strata which would give them information about the
beginnings of formation of the continental ice sheet. This was thought to
have occurred about 30 million years ago. When the project had to be
terminated this season they had drilled through strata which date to about
22 million years. Analysis of this material indicated that the sediments
were consistent with what would be expected if glaciation had been a factor
in their deposition. This can be deduced by the deposition patterns and
the composition and distribution of rocks in these sediments. They
therefore had not reached strata which predate the ice sheet before the
project had to be shut down. Next year they will try again.
Things to ponder:
Research how scientists use coring techniques to learn about rock strata.
Contact the TEA in the field at
.
If you cannot connect through your browser, copy the
TEA's e-mail address in the "To:" line of
your favorite e-mail package.
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