Abstract:

This Digital Surface Model (DSM) is created using linear interpolation applied on highest return per unity ground, as acquired during the LiDAR campaign. The helicopter-based survey of the Rio San Francisco catchment has been conducted in the periods of March 7-17, 2012 and November 12-19, 2012. Coordinate System UTM, Datum WGS84, Zone 17S, and Geoid EGM96 - for orthometric height - are used. The horizontal accuracy is within 5cm (based on control landmark of the IGM geodetic network). Quality assurance is done by visually inspection and correction of classification and ghost reflections. Additional quality control is done for completeness of the point cloud density and for models creation, which assured internal consistency of terrain representation (removal of artifacts due to misclassification) and seamless integration between tiles. Total data extent, considering all tiles is W: 704190.00, S: 9552910.00, N: 718190.00, E:9564110.00. The DSM has the spatial resolution of 1m. The LiDAR survey has been carried out under the working group of Prof. J. Bendix. Operational support and quality check: Jörg Zeilinger, Brenner Silva, Thomaz Lotz

Abstract:

Abstract:

Quality controls applied to the hourly time series of the El-Tiro-climate stations. Temeprature and wind direction had to be adjusted for apparent deviations. for details review the file qualityassessment.pdf supplied with the ECSF best estimate data set

Abstract:

Please dont use this dataset anymore! Refer to ECSF climate data best estimate ver. 2 (ID 1415). This data set remains for reference only.
old abstract:
Quality assessment ECSF climate station hourly data:
Version 1; Advise: There are known errors in the precipitation record from June to November 2014. A new version with extended time span will be uploaded soon. Please be aware, that aggregated values may be wrong, due to the data gaps. This is especcially critical for precipitation.
By Rütger Rollenbeck, 16.3.2015, rollenbeck@lcrs.de
Variables: 
Ta2m =Air Temperature at 2 m (T)
PCP = Precipitation at 1 m (P)
Huma_2m = relative humidity at 2m (rH)
Irradiation = global radiation at 2 m (gRad)
Emitted radiation, Wind speed, wind direction and soil-temperatures are not yet published

For each variable, a measure of uncertainty is given in the original dimension. This value can be considered as the potential deviation from real conditions. Where no parallel measurements exist, the uncertainty is given as the standard deviation of that difference.

Abstract:

Weekly bulk samples of Forest soil water (1825 m.a.s.l) collected at three depths (10, 25 and 40 cm) for the analysis of stable isotopes (Oxygen-18 and Deuterium). The water isotopic composition was analyzed by wavelength-scanned cavity ring down spectroscopy (WS-CRDS) with a precision of 0.1 ‰ for Oxygen-18 and 0.5 for Deuterium (PicarroL1102-i, CA, US).

Abstract:

Weekly bulk samples of Forest soil water (2000 m.a.s.l) collected at three depths (10, 25 and 40 cm) for the analysis of stable isotopes (Oxygen-18 and Deuterium). The water isotopic composition was analyzed by wavelength-scanned cavity ring down spectroscopy (WS-CRDS) with a precision of 0.1 ‰ for Oxygen-18 and 0.5 for Deuterium (PicarroL1102-i, CA, US).

Abstract:

Weekly bulk samples of Pasture soil water (1975 m.a.s.l) collected at three depths (10, 25 and 40 cm) for the analysis of stable isotopes (Oxygen-18 and Deuterium). The water isotopic composition was analyzed by wavelength-scanned cavity ring down spectroscopy (WS-CRDS) with a precision of 0.1 ‰ for Oxygen-18 and 0.5 for Deuterium (PicarroL1102-i, CA, US).

Abstract:

Hand-Dip Sampling for the collection of spring water for the analysis of stable isotopes (Oxygen-18 and Deuterium). The water isotopic composition was analyzed by wavelength-scanned cavity ring down spectroscopy (WS-CRDS) with a precision of 0.1 ‰ for Oxygen-18 and 0.5 for Deuterium (PicarroL1102-i, CA, US).

Abstract:

Hand-Dip sampling for the collection of surface water for the analysis of stable isotopes (Oxygen-18 and Deuterium). The water isotopic composition was analyzed by wavelength-scanned cavity ring down spectroscopy (WS-CRDS) with a precision of 0.1 ‰ for Oxygen-18 and 0.5 for Deuterium (Picarro L1102-i, CA, US).

Abstract:

Hand-Dip sampling for the collection of surface water for the analysis of stable isotopes (Oxygen-18 and Deuterium). The water isotopic composition was analyzed by wavelength-scanned cavity ring down spectroscopy (WS-CRDS) with a precision of 0.1 ‰ for Oxygen-18 and 0.5 for Deuterium (PicarroL1102-i, CA, US).