• Home
• About
  • About the project
  • Approach
  • Study area
  • Subprojects
  • Contact
  • DFG Science TV
  • ECSF virtual field trip
• Staff
• Publications
  • List publications
• Documents and Services
  • General Information
• Data
  • List datasets
  • Category tree
  • Plots of climate datasets
• RESPECT Phase 1
  • About the project
  • Approach
  • Study area
  • Subprojects
  • Staff
  • Contact
  • DFG Science TV
  • General Information
• PAK 823-825(2013-2018)
  • Overall aims
  • Structure
  • Subprojects
  • Staff
  • Counterparts
  • Study area
  • Contact
  • Links
  • News
  • Data agreement
• FOR816/2(2010-2013)
  • Overall aims
  • Structure
  • Subprojects
  • Staff
  • Counterparts
  • Study area
  • Contact
  • Links
  • FOR816 Data user agreement

Platform data

Overview

Detailed view

Long term series of weekly total of incident pricipitation (mean of 5 replicates), pH and EC of bulked PCP samples.
NOTE: PCP volumes from > April 2003 need to be quality checked (rate 50 to 20). 

Taken from Fleischbein et al. (2005):
Rainfall interception in forests is influenced by properties of the canopy that tend to vary over small distances. Our objectives were: (i) to determine the variables needed to model the interception loss of the canopy of a lower montane forest in south Ecuador, i.e. the storage capacity of the leaves S and of the trunks and branches S-t, and the fractions of direct throughfall p and stemflow p(t); (ii) to assess the influence of canopy density and epiphyte coverage of trees on the interception of rainfall and subsequent evaporation losses.
The study site was located on the eastern slope of the eastern cordillera in the south Ecuadorian Andes at 1900-2000 m above sea level. We monitored incident rainfall, throughfall, and stemflow between April 1998 and April 2001. In 2001, the leaf area index (LAI), inferred from light transmission, and epiphyte coverage was determined.

The mean annual incident rainfall at three gauging stations ranged between 2319 and 2561 mm. The mean annual interception loss at five study transects in the forest varied between 591 and 1321 mm, i.e. between 25 and 52% of the incident rainfall. Mean S was estimated at 1(.)91 mm for relatively dry weeks with a regression model and at 2(.)46 mm for all weeks with the analytical Gash model; the respective estimates of mean S-t were 0(.)04 mm and 0(.)09 mm, of mean p were 0(.)42 and 0(.)63, and of mean pt were 0(.)003 and 0(.)012. The LAI ranged from 5(.)19 to 9(.)32. Epiphytes, mostly bryophytes, covered up to 80% of the trunk and branch surfaces. The fraction of direct throughfall p and the LAI correlated significantly with interception loss (Pearson's correlation coefficient r = -0(.)77 and 0(.)35 respectively, n = 40). Bryophyte and lichen coverage tended to decrease S, and vascular epiphytes tended to increase it, although there was no significant correlation between epiphyte coverage and interception loss. Our results demonstrate that canopy density influences interception loss but only explains part of the total variation in interception loss. Copyright (c) 2004 John Wiley & Sons, Ltd.

Long term series of weekly total of incident pricipitation (mean of 5 replicates), pH and EC of bulked PCP samples.
NOTE: PCP volumes from > April 2003 need to be quality checked (rate 50 to 20).

Beschreibung: Hier sind die Ergebnisse der Auswertungen der hemisphärischen Bilder mit dem Programm HemiView Canopy Analysis Software (Version 2.1 SR1, Delta T Devices Ltd., www.delta-t.co.uk) angegeben.
Weiterhin sind die Ergebnisse der Vermessungen an den Messpunkten angegeben.
In der Übersicht sind die Mittelwerte (Zeile 6-14), die Standardabweichungen (Zeile 23-31) und die Variationskoeffizienten (Zeile 40-48) angegeben.
Qualität: Mittelwerte aus den Rohdaten (9 Einzelmessstellen im Plot)
Angegebene Literatur: Anderson, M.C. 1964a. Light relations of terrestrial plant communities and their measurement. Biological Reviews 39:425-486. 
Anderson, M.C. 1964b. Studies of the woodland light climate I. The photographic computation of light condition. Journal of Ecology 52:27-41. 
Anderson, M.C. 1964c. Studies of the woodland light climate. II. seasonal variation in the light climate. Journal of Ecology 52:643-663. 
Campbell, G.S. 1986 Extinction coefficients for radiation in plant canopies calculated using an ellipsoidal inclination angle distribution. Agricultural & Forest Meteorology, 36:317 - 321.

Original data: FOR402 (Phase 2) ID: 50655-50663; Creators: Dalitz, Helmut and Oesker, Mathias (AG:  B2-B2)
 
This dataset has been migrated from the previous FOR402-Database to the FOR816-Database by the Central Data Management Z1/FOR816.
Please keep in mind that the migration included all avilable metainfomation which were accessible through the FOR402-Database. Nevertheless, it can't be guaranteed that no thematic misinterpretation occured in the data/attribute description.
There has been no further disciplin specfic control. In any case of ambiguity please contact the dataset creator.

Weekly time series of precipitation data from the ECSF area at the measuring station FN2 located at the intersection of Camino Canal and Camino Zig-Zag. Precipitation was measured with 5 Hellmann-type pluviometers. The resulting weekly replicates of precipitation were volume-weighted and bulked to one sample per collecting interval. Electrical conductivity and pH values were measured immediately in unfiltered aliquots in the laboratory at the ECSF.

Weekly time series of precipitation data from the ECSF area at the measuring station FN3 located on T2 near the ECSF meteorological station. Precipitation was measured with 5 Hellmann-type pluviometers. The resulting weekly replicates of precipitation were volume-weighted and bulked to one sample per collecting interval. Electrical conductivity and pH values were measured immediately in unfiltered aliquots in the laboratory at the ECSF.

Weekly time series of water fluxes, electrical conductivity, pH values and measured concentrations of Al, Mn, Zn, Cl, PO4-P, Total P, NH4-N, NO3-N, Total N, K, Na, Mg, Ca and Total organic C in precipitation from the Bombuscaro site at 1000 m a.s.l. located at the climate station. The weekly time series extends between March 2018 and December 2019. Precipitation was sampled with 5 Hellmann-type collectors. Replicates were collected, volume-weighted and bulked to one sample per plot. Electrical conductivity and pH values were measured immediately in unfiltered aliquots in the laboratory at the ECSF. Samples were filtered (4-7 µm) in the laboratory of the ECSF and stored at -20 °C until transport in frozen state to Germany for concentration measurements.