LAKE FRYXELL METEOROLOGICAL STATION
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Photo taken by Thomas Nylen - 2002/2003 Season
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| MCM LTER Data Manager: | Chi Yang |
| Address: | Institute of Arctic and Alpine Research, Campus Box 450, University of Colorado Boulder, Colorado 80309-0450 |
| Phone: | (303) 492-4639 |
| E-Mail: | Chi.Yang@colorado.edu |
| PRINCIPAL INVESTIGATOR: | Andrew G. Fountain |
| Address: | Department of Geology, Portland State University, Portland OR, 97207-0751 |
| Phone: | (503)725-3022 |
| E-Mail: | fountaina@pdx.edu |
| OTHERS: | Thomas Nylen |
| Address: | Department of Geology, Portland State University, Portland OR, 97207-0751 |
| Phone: | (503)725-3355 |
| E-Mail: | nylent@pdx.edu |
ABSTRACT: As part of the Long Term Ecological Research in the McMurdo Dry Valleys of Antarctica, meteorological data was collected from various locations throughout Taylor, Wright and Victoria Valleys. These files contain data for the Lake Fryxell meteorology station (in Taylor Valley).
VARIABLES: Samples are represented using the following variable
names:
| Variable Name | Description |
| Dataset Code | Code for given set of information from Lake Fryxell Met Station |
| MetLocID | Location code for Lake Fryxell meteorology station |
| Date | Date/time of sample (McMurdo time) |
| AirT3m | Average air temperature at 3 m above ground |
| AirTMax | Maximum air temperature at 2.5 - 3 m above ground |
| AirTMin | Minimum air temperature at 2.5 - 3 m above ground |
| AirTdel3m1 | Air temperature at 3 m above ground minus air temperature at 1 m above ground |
| AirT Comments | Comments about air temperature |
| RichNo | Bulk richardson number |
| RichNo Comments | Comments about bulk richardson number |
| RH | Relative humidity |
| RH Comments | Comments about relative humidity |
| SoilT0cm | Soil temperature at 0 cm depth |
| SoilT5cm | Soil temperature at 5 cm depth |
| SoilT10cm | Soil temperature at 10 cm depth |
| SoilT Comments | Comments about soil temperature |
| PAR | Photosynthetically active radiation |
| SwRadIn | Incoming shortwave radiation |
| SwRadOut | Outgoing shortwave radiation |
| Radiation Comments | Comments about radiation measurements (PAR, shortwave) |
| WDir | Average wind direction |
| WDirStD | Standard deviation of wind direction |
| WSpd | Wind speed |
| WSpdMax | Maximum wind speed |
| WSpdMin | Minimum wind speed |
| Wind Comments | Comments about wind speed |
| WVapD | Water vapor density |
| WVapD Comments | Comments about water vapor density |
| Snow Height | Depth of snow |
| Snow Height Comments | Comments about depth of snow |
RESEARCH LOCATION: The Lake Fryxell meteorology station is located at a latitude of 77 10.6 S, a longitude of 163 10.1766 E, and an elevation of 19 meters above sea level. As of 8-Dec-1998, the station was 1 meter above Lake Fryxell. Descriptions of this and other McMurdo Dry Valley meteorology stations can be found at http://huey.colorado.edu/LTER/datasets/meteorology/metlocs.html.
METHODS: When the McMurdo Dry Valley LTER project began in December, 1993, a lake-ice meteorology station was already set up at Lake Fryxell. It was a 6 foot tower built by Rich Harnish in ~1989, but had not collected data for at least a year. Peter Doran, noting that the problem was power related (since the battery was under water and the voltage was less than 5), righted the station, and rebuilt it with new power supply, a new wind monitor, new CR10, new solar panel, and added a quantum sensor. The under water light sensors were not hooked up again nor was the barometric pressure sensor.
The lake-ice station was operated from 7 December 1993 to 6 January 1994. At that time, it was decided that maintenance of the records at the site of the old Fryxell land station was more important than the ice station so the ice station was cannibalized to re-establish the Lake Fryxell shore station, (which had been destroyed by wind the previous winter). The station was based on a 6 foot tripod which set it apart from the other Taylor Valley stations, but a 10 foot tower was subsequently installed in year 2. The land station is located a few meters above the old site to avoid rising lake levels.
On June 25, 2001 @ 0230 the station mast broke and blew over, breaking the wind monitor. Station was taken apart on November 16, 2001, with the sensors except wind temporally set up on what was left of the station. On November 27, 2001 the station was reconstructed and was made operational again. Mark all values from June to November as bad or questionable except the soil temperatures
The station was set up to sample sensors every 30 seconds and send summary statistics (for example, averages and maximums) to solid-state storage modules every:
Measurement |
Starting Season |
Ending Season |
Instrument Used |
| Air temperature @ 3 m |
1999/2000 |
--- |
Campbell Scientific 207 temp/rh probe Campbell Scientific 107 temp probe |
| Air temperature difference between 1 m & 3 m heights |
|
|
Chromel-constantan thermocouple wire |
| Relative humidity @ 3 m |
1999/2000 |
--- |
Campbell Scientific 207 temp/rh probe Vaisala HMP45C RH probe |
| Soil temperature @ 0 cm |
|
|
Campbell Scientific 107B temperature probe |
| Soil temperature @ 5 cm |
|
|
Campbell Scientific 107B temperature probe |
| Soil temperature @ 10 cm |
|
|
Campbell Scientific 107B temperature probe |
| Wind speed |
|
|
R.M. Young model 05103 wind monitor |
| Wind direction |
|
|
R.M. Young model 05103 wind monitor |
| Solar Flux (incoming) |
|
|
LI-COR model L1200S silicon pyranometer |
| Solar Flux (outgoing) |
|
|
LI-COR model L1200S silicon pyranometer |
| PAR |
|
|
LI-COR model 190SB quantum sensor |
| Snow Height |
2002/2003 |
|
Campbell Scientific SR50 Sonic Ranging Sensor |
TIMING: Data was gathered from the Lake Fryxell meteorology station on the dates and frequencies listed
in the link below. Due to regular station maintenance, occasional short gaps
(hours) with missing data occurs. Longer intervals (several months) with missing
data have occasionally occurred due to storage module problems, but this is
minimized through the regular station upkeep every austral summer.
Click here to see the dates and frequencies.
CITATIONS: Doran, Peter T., Gayle L. Dana, Jordan T. Hastings and Robert A. Wharton, Jr. 1995. McMurdo Dry Valleys Long-Term Ecological Research (LTER): LTER automatic weather network (LAWN). Antarctic Journal of the U.S. 30(5): 276-280.
COMMENTS: Meteorological data is collected year-round at each of the stations in the McMurdo Dry Valleys of Antarctica.
After retrieving this data (usually every January), the parameters that are recorded are processed from level 0 (raw) to level
1 (processed, provided on the web). The
raw data file descriptions and task lists summarize what was done to get from level 0 to level 1.
STATUS: Public Access (Type 1).
VARIABLE DESCRIPTION:
|
variable |
type |
description |
units |
missing value indicator |
minimum |
maximum |
precision |
|
Dataset code |
Text |
Code for given set of information for Lake Fryxell meteorology station |
None |
Required entry |
n/a |
n/a |
n/a |
|
MetLocID |
Text |
Location code for Lake Fryxell meteorology station |
None |
Required entry |
n/a |
n/a |
n/a |
|
Date |
Date |
Date/time of sample (McMurdo time) |
MM/DD/YY HH24:MM |
Required entry |
12/01/94 00:00 |
12/31/04 23:59 |
MM (minutes) |
|
AirT3m |
Number |
Average air temperature at 3 m above ground |
degrees celcius |
Null |
-70 |
15 |
0.01 |
|
AirTMax |
Number |
Maximum air temperature at 2.5 - 3 m above ground |
degrees celcius |
Null |
-70 |
15 |
0.01 |
|
AirTMin |
Number |
Minimum air temperature at 2.5 - 3 m above ground |
degrees celcius |
Null |
-70 |
15 |
0.01 |
|
AirTdel3m1 |
Number |
Air temperature at 3 m minus air temperature at 1 m |
degrees celcius |
Null |
n/a |
n/a |
0.01 |
|
AirT Comments |
Text |
Helpful hints on air temperatures |
None |
Null |
n/a |
n/a |
n/a |
|
RichNo |
Number |
Bulk Richardson Number |
|
Null |
n/a |
n/a |
0.1 |
|
RichNo Comments |
Text |
Helpful hints on Bulk Richardson number |
None |
Null |
n/a |
n/a |
n/a |
|
RH |
Number |
Relative humidity |
percent |
Null |
0 |
100 |
0.1 |
|
RH Comments |
Text |
Helpful hints on relative humidity |
None |
Null |
n/a |
n/a |
n/a |
|
SoilT0cm |
Number |
Soil temperature at 0 cm depth |
degrees celcius |
Null |
-70 |
25 |
0.01 |
|
SoilT5cm |
Number |
Soil temperature at 5 cm depth |
degrees celcius |
Null |
-70 |
25 |
0.01 |
|
SoilT10cm |
Number |
Soil temperature at 10 cm depth |
degrees celcius |
Null |
-70 |
25 |
0.01 |
|
SoilT Comments |
Text |
Helpful hints on soil temperatures |
None |
Null |
n/a |
n/a |
n/a |
|
PAR |
Number |
Photosynthetically active radiation |
µmols/second/meter2 |
Null |
0 |
2000 |
0.1 |
|
SwRadIn |
Number |
Incoming shortwave radiation/solar flux |
W/m2 |
Null |
0 |
900 |
0.1 |
|
SwRadOut |
Number |
Outgoing shortwave radiation/solar flux |
W/m2 |
Null |
0 |
900 |
0.1 |
|
Radiation Comments |
Text |
Helpful hints on photosynthetically active, shortwave & longwave radiation/solar flux measurements |
None |
Null |
n/a |
n/a |
n/a |
|
WDir |
Number |
Average wind direction |
degrees from north |
Null |
0 |
360 |
0.1 |
|
WDirStD |
Number |
Standard deviation of wind direction |
degrees from north |
Null |
0 |
n/a |
0.1 |
|
WSpd |
Number |
Wind speed |
meters per second |
Null |
0 |
n/a |
0.1 |
|
WSpdMax |
Number |
Maximum wind speed |
meters per second |
Null |
0 |
n/a |
0.1 |
|
WSpdMin |
Number |
Minimum wind speed |
meters per second |
Null |
0 |
n/a |
0.1 |
|
Wind Comments |
Text |
Helpful hints on wind measurements |
None |
Null |
n/a |
n/a |
n/a |
|
WVapD |
Number |
Water Vapor Density |
|
Null |
n/a |
n/a |
0.1 |
|
WVapD Comments |
Text |
Helpful hints on water vapor density measurements |
None |
Null |
n/a |
n/a |
n/a |
Snow Height |
Number |
Sonic ranger measurement of surface |
cm |
Null |
n/a |
n/a |
0.1 |
|
Snow Height Comments |
Text |
Helpful hints on snow depth |
None |
Null |
n/a |
n/a |
n/a |
FLAGS: Flags used during data processing:
"#": Bogus value, initialized but never calculated
"B": Recorded by instrument,but known to be "bad data"
"F": Recorded by instrument, but apparently flawed
"M": Supposedly recorded by instrument, but missing
"N": Not available/applicable (e.g. WDir when WSpd=0)
"R": Out of Range (user-adjustable limits)
"*": Subjectively voided
In addition, flags were found that were not included in the list above. Peter Doran was therefore contacted to find out how to translate the flags for "S", "U" and "V". He advised to use the following:
"S": Negative value generated by noise in the system zeroed out (eg. incoming shortwave radiation level should not be negative, so convert negative value to zero)
"U": Constant ice surface ablation on the glaciers causes the 20-centimeter ice temperature probe to continually become shallower. The probe depth is therefore not well known.
"V": Constant ice surfaceablation on the glaciers causes the 1-meter ice temperature probe to continually become shallower. The probe depth is therefore not wellknown.
Since the flags in the data files were added to values that were recorded, rather than appearing as a separate variable (eg. 0.0N, as opposed to 0.0, N), it was necessary for the data manager to revise these files so that the measurements were represented in numeric format & the flags would be in text format. Denise Steigerwald therefore imported the data into Microsoft Access, created comment fields for categories such as air temperature, humidity, wind, radiation, and soil temperature, and moved the suffixes described above to these comments fields. The comments were then expanded from the single letter codes to short descriptions of what was occurring.