5 July, 2000
July 5, 2000
Matanuska Glacier, Alaska
Not long after the sun dips behind the Talkeetna Mountains to the west and north the air takes a noticeable drop in temperature and clouds begin to form around the mountains. When morning rolls around the mountains seem fully enclosed in clouds and there’s a good chill in the air. As a result the workdays starts a bit later in order to take advantage of better temperatures. Usually it is a goal to get out by 9:00 in the morning and earlier only if there’s a pressing need for it. Temperatures rise and remain at a very comfortable level into the early evening hours. This morning a constant but light rain was falling and although everyone was awake and ready to go out for the day, we held back to see if the sun might burn off some clouds and lighten things up a bit. However, an ISCO water sampler needed attention before noon and so we headed out in the rain at 10:00 to the north vent station.
A vent is a location near the terminus of the glacier where there is an upward discharge of water that has been flowing in and under the glacier and is now coming out to create surface runoff. There are a number of these large vents on the Matanuska glacier and each is referred to with a different name for obvious reasons. The water coming out of a vent is under fairly high pressure due to the weight of all the water in the subglacial drainage system above that feeds into it. This results in water coming out that is supercooled and freezes upon reaching “normal” pressures at the surface. A supercooled liquid is one whose temperature in the liquid state is below the “normal” freezing point. This commonly occurs to liquids under pressure. When the pressure drops to normal, the liquid begins to freeze to some extent. This same phenomenon is observed occasionally when you open a really cold soft drink. Soon after opening the container the drink begins to get slushy as the supercooled liquid starts to freeze under the lowered pressure.
When visiting an ISCO station one problem to watch for, and a serious one at that, is that the instruments that have been placed in the vent can get frozen in place. At a number of these stations other data collecting devices are attached with the ISCO collection tube and could be frozen in with it. At stream side stations there is always a watchful eye kept on rising stream levels as the melting increases into the summer season. Quite often the ISCO must be moved to higher ground. In addition, some of the vents are surging out right at the edge of unstable ice ledges and a concern is for a section of the ice to break off and wash downstream. At these stations the ISCO is kept a fair distance from the edge and longer lengths of tubing are used to draw in the water sample. It is also essential to check that the instrument is still powered and operating correctly.
The ISCO is a device that can be programmed to collect up to 24 unique water samples through tubing that connects from the device to the water source. It looks like a very large industrial size vacuum cleaner. Currently the ISCO’s in place at various stations are collecting samples every two hours and must be visited every two days in order to install a fresh set of empty sample bottles and check for any problems. At some stations, daily visits are required to check for some of the problems mentioned earlier. Ben and I will be utilizing these devices in our research and this morning we learned about their operation and things to watch for when checking up on them. There’s still more features of the glacier to explore and learn about before we can begin our research. Tomorrow we’ll find out more about this massive river of ice. Till then.....
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