i-Box Hochhaeuser
North-facing slope site (CS-NF27)
Description
The Innsbruck Box (i-Box) is a testbed for studying boundary layer processes in highly complex terrain. Designed to be a long-term "reference box" for studying the characteristics of turbulence structure and exchange processes in truly complex topography, i-Box represents an integrated approach combining three-dimensional long-term turbulence observations with high-resolution numerical modeling. The i-Box observational stations are located in the Inn Valley, an approximately northeast-southwest oriented valley in western Austria, characterized by very complex terrain with steep slopes, flat foothills, numerous side valleys, and variable land use characteristics. The locations of the core sites (six turbulence stations) were chosen to represent different topographic features in order to secure the universality of the obtained results. Further information about the i-Box project can be found in Rotach et al. (2017) and on the i-Box WIKI.
Site CS-NF27 is located on a steep slope on the south sidewall of the Inn Valley. The site is characterized by a relatively homogeneous and approximately 400-m long stretch of alpine meadow, with a line of trees to either side of the slope at a distance of about 70 m. A forest starts about 250 m farther up the slope and a small road crosses the slope immediately below the station. The 6-m high tower is a full energy-balance station and is instrumented with two levels of turbulence measurements (one level before September 2017).
Site characteristics
Coordinates: 47.28755˚N, 11.63122˚E (UTM: 698958.75 E, 5240477.18 N)
Altitude: 1009 m MSL
Slope angle: 27˚
Slope orientation: 1˚
Surface characteristics: alpine meadow
Status: operational since August 2013 (the station was not running between 2 November 2016 and 04 September 2017)
Power supply: solar panel
Datalogger: CR1000
History/logbook: logbook and data availability
Instrumentation
Instrument | Height | Serial number | Notes |
---|---|---|---|
Turbulence | |||
CSAT3 | 1.5 m | 2293 | Since 05 Sep 2017 Angle to true north: 260˚ |
CSAT3 | 6.8 m | 2293 | until 02 Nov 2016 Angle to true north: 260˚ |
Campbell KH20 | 6.8 m | 1698 | until 02 Nov 2016 Path length: 0.01267 m Path separation: 0.17 m xkw: -0.187 ln(mV)m3/g Intercept: 3258 mV |
Irgason | 7.08 m | 1343 | since 05 Sep 2017 Angle to true north: 260˚ |
Temperature/Humidity | |||
Rotronic HC2-S3 | 6.83 m | ||
Wind | |||
Anderaa cup anemometer | 1.47 m | Anderaa 1284 | |
Anderaa cup anemometer | 2.62 m | unreadable | |
Anderaa cup anemometer | 5.33 m | Anderaa 1285 | |
Anderaa windvane | 1.51 m | W200P | |
Pressure | |||
Setra 278 | 4991772 | in logger box | |
Precipitation/Snow | |||
SR50A | 1.20 m | CS7212(1019) | |
Rain gauge | 16 Nov 2018 - 21 Jan 2019 | ||
Radiation | |||
CNR4 | 2.00 m | 110705 | SWd: 13.05 uV/Wm2 SWu: 10.06 uV/Wm2 LWd: 13.26 uV/Wm2 LWu: 13.72 uV/Wm2 |
Soil | |||
Heat Flux Plate HFP01 | 10 cm | 13619 | 60.74 uV/Wm2 |
Trime PICO64 | 5 cm | 35250 | |
Campbell 107 Temp probe | 2 cm | ||
Campbell 107 Temp probe | 5 cm | ||
TDT Soil moisture | 7 cm |
Datasets
- RAWDATA since 2017
- Uncorrected 1-min raw data since Sep 2017, no quality checks applied
- RAWDATA until 2016
- Uncorrected 1-min raw data until Nov 2016, no quality checks applied
- RAIN
- Uncorrected 1-min precipitation and snow depth data, no quality checks applied
- RADIAT1
- 1-min radiation data after applying the respective calibration coefficients to the uncorrected raw data; no quality checks applied
- FLUXL1AND2 since 2017
Processed turbulence data with an averaging interval of 30 min (processing was performed using EdiRe)
Processing includes despiking; double-rotation of the wind components; detrending with a recursive filter and a time constant of 200 s; and applying frequency-response corrections, heat-flux corrections for humidity effects, oxygen corrections for KH20, and WPL corrections. The datafile contains several quality flags.
- FLUXL1 until 2016
Processed turbulence data with an averaging interval of 30 min (processing was performed using EdiRe)
Processing includes despiking; double-rotation of the wind components; detrending with a recursive filter and a time constant of 200 s; and applying frequency-response corrections, heat-flux corrections for humidity effects, oxygen corrections for KH20, and WPL corrections. The datafile contains several quality flags.
- ZEROPLANE
Annual cycle of zero-plane displacement height (Sfyri et al. 2018)
d = (-4.3574e-06*jd^2+0.0016*jd-0.0061) for jd = 1 Jan - 31 Dec