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).

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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:

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