Senator Beck Study Plot
37°54'24.77918"N, -107°43'34.55556"W; 12,186'
Near-Real Time Mountain System Monitoring Data for the Senator Beck Study Plot (SBSP)
The following are provisional data collected and displayed directly from instrumentation in Senator Beck Basin. These data have not undergone rigid quality control procedures, and should be used solely for informational purposes.
• Wind Data:
24-Hour Wind Summary
• Graphical Wind Rose: 1hr | 12hr | 24hr
• Temperature & RH Data:
24-Hour Temp Summary
• Radiation Data: Hourly | 24-Hour Summary
• Snowpack data will return Oct 1, 2013
Senator Beck Study Plot (SBSP) is located at a level site near the center of the Senator Beck Basin Study Area at 12,186’ (3714m), above treeline and in the alpine tundra. The SBSP consists of a single
10 meter tower, with an extensive array of instrumentation, and an adjoining
12m x 36m snow profile plot. Signage advises the general public to avoid approaching
the mast or entering the snow profile plot and cooperation has been excellent.
Data is acquired via RF link.
This very exposed location is subject to the full force of the alpine winds inside the Basin and, as such, measurements of wind speed and direction are reasonably representative of wind-effected snowcover formation and other processes within the Basin. Because of these dominant wind effects, SBSP is a poor location for measuring precipitation – a very large portion of snowfall would simply blow over the top of the precipitation collector – and no precipitation measurements are made. Measurements of snowpack depth at SBSP are understood to be simply ‘point’ measurements that cannot be reliably extrapolated any distance to estimate snow depth in the surrounding alpine terrain; these measurements are meaningful only as a time series of snow depth at that point. Because the site sits on a level bench near the middle of the Senator Beck Basin watershed, air temperature and humidity data from SBSP are minimally affected by the surrounding terrain and often present a smaller diurnal range than at the Swamp Angel Study Plot. The terrain horizon to the east, south, and west is sufficiently low and open to enable meaningful measurements of incoming solar radiation and of outgoing long wave radiation emitted from the snowpack surface.
Wind speed and direction are measured at SBSP at the top of the 30’ tower, minimizing the influence of the immediate terrain. Snowpack depth, also referred to as height-of-snow (HS), is measured, in meters, at the end of each hour by an ultrasonic distance sensor designed for monitoring HS. Air temperature (Celsius) and relative humidity (percent) are measured every five seconds at a fixed height on the tower. Incoming short- and long-wave radiation values are measured, in watts per square meter, every five seconds by individual sensors at the top of the tower. A proxy for long-wave radiation emitted from the snowpack surface is monitored by measuring the snowpack surface temperature (Celsius) every five seconds using a sophisticated infrared temperature sensor specifically designed for snow measurements. All these five-second measurements are averaged each hour to generate 1-hour data, and again once every 24 hours, at midnight, to generate 24-hour ‘summary’ data. Times reported are in Mountain Standard Time; we do not utilize daylight savings time.
SBSP is, by choice,
an exposed alpine site subject to winds of up to 90+ mph (40+ m/s). Wind effects
are often present on the snow surface surrounding the mast. Trico Peak (13,321',
4,060m) is seen in the background, looking west. The single 40 watt photovoltaic panel seen at mid-mast
charges a 400 amp-hour battery bank contained in a sub-snow-surface enclosure
located some 10 meters from the mast.
Horizontal 'stiff arms' extending from the mast enable the transition from angled to vertical guywires to the ground anchors, thereby eliminating nearly all snow settlement stresses on the mast's guywires yet still providing a stable mast in high winds.
A hexagonal array of vertical,
3m (9.8') 'height-of-snow' (HS) measurement stakes is deployed around and
7.5m (24.6') from the mast to enable calculation of snow surface slope and
aspect, improving the interpretation of reflected radiation being measured
by the down-looking pyranometers. These HS stakes are read using binoculars,
leaving the snow undisturbed.
At the top of the SBSP mast are deployed a wind monitor (RM Young™ Model 05103-5), two up-looking, full-range pyranometers (Kipp & Zonen CM21, 305-2800 nm (50% points)), a third filtered pyranometer (Kipp & Zonen™ CM21 with RG695 filter dome, 780-2800 nm (50% points)), and a pyrgeometer (Kipp & Zonen™ CG4). One of the full-range up-looking pyranometers is deployed with a fixed shadow band for measurements of diffuse radiation at solar noon. The shadow post is modeled upon the Swiss's Alpine Surface Radiation Budget project specifications. Air temperature and humidity are monitored just below the level of the radiation sensors (Campbell Scientific™ CS500).
A view of the
lower end of the mast looking up the south side of the mast shows the
system's Campbell Scientific™ CR10x dataloggers (two) enclosure (white
cabinet) located at 9.5' (2.9m) above the ground; a separate multiplexer
enclosure is located just below the dataloggers, out of view. On the arm
extending due south from the mast are mounted an ultrasonic snow depth
sensor (Campbell Scientific™ SR50), two down-looking pyranometers measuring
reflected radiation from the snow surface (a Kipp & Zonen CM21, 305-2800 nm
(50% points) and a Kipp & Zonen™ CM21 with RG695 filter dome, 780-2800 nm
(50% points)) and an infra-red snow surface temperature sensor (AlpuG
GmbH™ SnowSurf) Another arm extending east and west from the mast houses, to the
east, an air temperature and humidity sensor (Campbell Scientific™ CS500)
and, to the west, a second wind monitor (RM Young™ Model 05103-5).
A snow temperature sensor array is deployed near the mast, with instrument leads housed in flexible steel conduit. The array consists of five Campbell Scientific™ 107 probes in a five-pronged, horizontal 'fork' array, with 10 cm of vertical spacing between sensors. The upper two sensors are visible in this photograph, and the remaining three sensors are beneath the snow surface. The array can be located at any desired level in the snowpack and re-positioned as the snowpack evolves. A wooden stake indicates depth to the center sensor in the array.
During the summer of 2005 we installed several soil monitoring sensors to the SBSP array: a soil heat flux plate (Rebs™ HFT3), a soil water content reflectometer (Campbell Scientific™ CS616), and soil temperature probes (Campbell Scientific™ 107).