LAKE BONNEY METEOROLOGICAL STATION
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Photo taken by Thomas Nylen - 1999-2000 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 Bonney 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 Bonney Met Station |
| MetLocID | Location code for Lake Bonney Met 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 |
| AirT Comments | Comments about air temperature |
| PAR | Photosynthetically active radiation |
| Ppt | Unevaporated precipitation |
| Ppt Comments | Comments about precipitation |
| 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 |
| LwRadIn* | Incoming longwave radiation based on applying instrument-specific multiplier |
| LwRadIn2* | Incoming longwave radiation calculated from thermopile, case thermistor and the dome or hemisphere thermistor measurements |
| LwRadOut* | Outgoing longwave radiation based on applying instrument-specific multiplier |
| LwRadOut2* | Outgoing longwave radiation calculated from thermopile, case thermistor and the dome or hemisphere thermistor measurements |
| SwRadIn | Incoming shortwave radiation |
| SwRadOut | Outgoing shortwave radiation |
| Radiation Comments | Comments about photosynthetically active, longwave &/or shortwave radiation |
| 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 |
* Note: see documentation on Procedures for Correcting Eppley Pyrgeometer Data for an explanation of the differences between LwRadIn/LwRadOut and LwRadIn2/LwRadOut2 measurements.
RESEARCH LOCATION: The Bonney meteorology station is located at a latitude of 77 50.981 S, a longitude of 162 27.84968 E, and an elevation of 64.43 meters above sea level. Descriptions of this and other McMurdo Dry Valley meteorology stations can be found at http://huey.colorado.edu/LTER/datasets/meteorology/metlocs.html.
METHODS: The Lake Bonney meteorology station was initially built on the lake's ice cover in November, 1993. Shortly thereafter the station was listed to the point where it was decided to move it to shore. Some attempt was made to right the station during this period. The move of the station was done using the ATV with the station still running. The move began at 14:50 and ended at 15:06 on December 17, 1993. Data collected after 15:06 was done so with the station in it's final position. The clock synchronized with John Priscu's logger measuring light on Nov 26 in afternoon. 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 |
| Relative humidity @ 3 m |
1999/2000 |
--- |
Campbell Scientific 207 temp/rh probe Vaisala HMP45C RH probe |
| Soil temperature @ 0 cm |
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Campbell Scientific 107B temperature probe |
| Soil temperature @ 5 cm |
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Campbell Scientific 107B temperature probe |
| Soil temperature @ 10 cm |
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Campbell Scientific 107B temperature probe |
| Longwave radiation |
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Eppley precision infrared radiometer (pyrgeometer) |
| Wind speed |
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R.M. Young model 05103 wind monitor |
| Wind direction |
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R.M. Young model 05103 wind monitor |
| Solar Flux (incoming) |
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LI-COR model L1200SZ silicon pyranometer |
| Solar Flux (outgoing) |
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LI-COR model L1200Z silicon pyranometer |
| PAR |
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LI-COR model 190SB quantum sensor |
| Precipitation |
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Belfort precipitation gage with BEl natural binary shaft encoder. Custom-made nipher shields provided by Canada's Atmospheric Environment Service. |
| Snow Height |
2002/2003 |
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Campbell Scientific SR50 Sonic Ranging Sensor |
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 Bonney meteorology station |
None |
Required entry |
n/a |
n/a |
n/a |
|
MetLocID |
Text |
Location code for Lake Bonney 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 |
n/a |
n/a |
0.01 |
|
AirTMax |
Number |
Maximum air temperature at 2.5 - 3 m above ground |
degrees celcius |
Null |
n/a |
n/a |
0.01 |
|
AirTMin |
Number |
Minimum air temperature at 2.5 - 3 m above ground |
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 |
|
PAR |
Number |
Photosynthetically active radiation |
µmols/ second/ meter2 |
Null |
n/a |
n/a |
0.1 |
|
Ppt |
Number |
Unevaporated precipitation |
millimeters |
Null |
n/a |
n/a |
0.1 |
|
Ppt Comments |
Text |
Helpful hints on precipitation |
None |
Null |
n/a |
n/a |
n/a |
|
RH |
Number |
Relative humidity |
percent |
Null |
n/a |
n/a |
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 |
n/a |
n/a |
0.01 |
|
SoilT5cm |
Number |
Soil temperature at 5 cm depth |
degrees celcius |
Null |
n/a |
n/a |
0.01 |
|
SoilT10cm |
Number |
Soil temperature at 10 cm depth |
degrees celcius |
Null |
n/a |
n/a |
0.01 |
|
SoilT Comments |
Text |
Helpful hints on soil temperatures |
None |
Null |
n/a |
n/a |
n/a |
|
LwRadIn |
Number |
Incoming longwave radiation based on applying instrument-specific multiplier |
W/m2 |
Null |
n/a |
n/a |
0.1 |
|
LwRadIn2 |
Number |
Incoming longwave radiation calculated from thermopile, case thermistor and the dome or hemisphere thermistor measurements |
W/m2 |
Null |
n/a |
n/a |
0.1 |
|
LwRadOut |
Number |
Outgoing longwave radiation based on applying instrument-specific multiplier |
W/m2 |
Null |
n/a |
n/a |
0.1 |
|
LwRadOut2 |
Number |
Outgoing longwave radiation calculated from thermopile, case thermistor and the dome or hemisphere thermistor measurements |
W/m2 |
Null |
n/a |
n/a |
0.1 |
|
SwRadIn |
Number |
Incoming shortwave radiation/solar flux |
W/m2 |
Null |
n/a |
n/a |
0.1 |
|
SwRadOut |
Number |
Outgoing shortwave radiation/solar flux |
W/m2 |
Null |
n/a |
n/a |
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 |
n/a |
n/a |
0.1 |
|
WDirStD |
Number |
Standard deviation of wind direction |
degrees from north |
Null |
n/a |
n/a |
0.1 |
|
WSpd |
Number |
Wind speed |
meters per second |
Null |
n/a |
n/a |
0.1 |
|
WSpdMax |
Number |
Maximum wind speed |
meters per second |
Null |
n/a |
n/a |
0.1 |
|
WSpdMin |
Number |
Minimum wind speed |
meters per second |
Null |
n/a |
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 |
grams per cubic meter |
Null |
n/a |
n/a |
0.1 |
|
WVapD Comments |
Text |
Helpful hints on water vapor density |
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.