Johannes Lüers

Description of the Waldstein Measuring Site

The chapter gives a brief overview of the measuring sites of the Bayreuth Center of Ecology and Environmental Research at the Waldstein mountain, Germany, northeast Bavaria, with a special focus on the Waldstein-Weidenbrunnen site (FLUXNET site DE-Bay) as well as the Pflanzgarten and Kohlerloh sites. The climate of the area, the structure of the forest stands with plant area index profiles, and the soil properties are described. There is a special focus on the tower installations, the permanent program, and the special experimental campaigns. Pictures of all sites and all relevant data are given, while the instrumentation is listed in Appendix A. Due to the storm event “Kyrill” in January 2007, the southern part of the forest was destroyed. A trace gas flux footprint analysis is presented for conditions after a large wind throw.

Development of Flux Data Quality Tools

At the Waldstein-Weidenbrunnen site, several techniques for data quality control were developed and tested and later on applied at European FLUXNET sites. The history of this development and the specific results for the site form the subject of this chapter. These data quality criteria include integral turbulence characteristics, which are dependent on heterogeneities in the footprint area and inside the canopy. Furthermore, footprint models were applied to determine the footprint climatology and to link these models with the data quality of eddy covariance data. This tool was also applied to find the optimal period for the application of the planar-fit rotation method. The energy balance closure was found to be about 80 % in all periods. These findings were summarized as a schema for data quality control and characterization of FLUXNET sites.

Improved data gap-filling schemes for estimation of net ecosystem exchange in typical East-Asian croplands

The estimation of carbon exchange between ecosystems and the atmosphere suffers unavoidable data gaps in eddy-covariance technique, especially for short-living and fast-growing croplands. In this study we developed a modified gap-filling scheme introducing a leaf area index factor as the vegetation status information based on the conventional light response function for two East-Asian cropland sites (rice and potatoes). This scheme’s performance is comparable to the conventional time window scheme, but has the advantage when the gaps are large compared to the total length of the time series. To investigate how the time binning approach performs for fast-growing croplands, we tested different widths of the time window, showing that a four-day window for the potato field and an eight-day time window for the rice field perform the best. The insufficiency of the conventional temperature binning approach was explained as well as the influence of vapor pressure deficit. We found that vapor pressure deficit plays a minor role in both the potato and the rice fields under Asian monsoon weather conditions with the exception of the early pre-monsoon growing stage of the potatoes. Consequently, we recommend using the conventional time-window scheme together with our new leaf-light response function to fill data gaps of net ecosystem exchange in fast-growing croplands.

Catchment Evapotranspiration and Runoff

The interplay between precipitation and evapotranspiration determines the input into the hydrological system of a catchment. Annual values of precipitation, evapotranspiration, and runoff measured at the catchment outlet for the 2002–2009 period were available. Annual precipitation clearly surmounted the sum of evapotranspiration and runoff. Part of the observed discrepancy might be due to the heterogeneity of precipitation and evapotranspiration within the catchment which has not been studied in sufficient detail. Annual evapotranspiration fluxes were remarkably constant during this period, whereas precipitation and runoff exhibited much larger interannual variability.

Climate, Air Pollutants, and Wet Deposition

One main topic of scientific and public interest regarding the Waldstein research site continues to be the high-quality observation of weather and air quality that captures the meteorology and climate of this particular site and the neighboring regions. Based on meteorological measurements made at the Waldstein facility from 1994 to the present, several studies—mainly of air temperature, precipitation, fog, wet deposition, and air pollutants—were conducted over the last 20 years. The expected strong global rise of earth’s basic air temperature will have a more moderated magnitude in Franconia, but the already continental location within the Central European climate zones, in combination with a heterogeneous landscape with imposed local orographic wind systems, will increase and reinforce diurnal and seasonal amplitudes and spatial variety of basic meteorological and air chemical elements and induce a higher risk of local extreme weather (climate) or smog (ozone) events. Forced by the change of macro- and mesoscale atmospheric circulation patterns across the northern hemisphere, the frequency and intensity of such weather-changing situations have increased during the last three or four decades in parallel with the span and the unpredictability of extreme weather conditions. That has, and will continue to have, an adjustment effect on air temperature and air humidity, sunshine duration and air pollution, wind (storm), date and duration of precipitation, and wet deposition of nitrogen, sulfur, salts, and metals and therefore a strong impact to the ecosystems at Waldstein.

Forest Climate in Vertical and Horizontal Scales

Microclimate was investigated within a heterogeneous spruce forest in Northern Bavaria, Germany, at the Waldstein–Weidenbrunnen site, especially during the EGER project in 2007, 2008 and 2011. Besides standard tower measurements, two innovative measuring techniques were used to investigate horizontal and vertical gradients. A particular focus was paid to advection within the homogeneous part and its effect on NEE, as well as gradients near a forest edge, measured by a mobile measuring system.

Long-Term Carbon and Water Vapour Fluxes

In this study we analyse eddy-covariance flux measurements of carbon dioxide and water vapour from 18 years at Waldstein–Weidenbrunnen (DE-Bay), a Norway spruce forest site in the Fichtelgebirge, Germany. Standard flux partitioning algorithms have been applied for separation of net ecosystem exchange NEE into gross primary production GPP and ecosystem respiration Reco, as well as gap-filling. The site has always been a carbon sink, and annual net uptake ( − NEE) shows a positive trend with values around 40 g C m−2 a−1 for 1997–1999 up to 615 ± 79 g C m−2 a−1 for 2011–2014. This is related to a strong increase in GPP, while Reco is slightly enhanced. Evapotranspiration increases coherently with NEE, while atmospheric demand, that is, potential evaporation, shows inter-annual variability, but no trend. Comparisons with studies from other warm-temperate coniferous forests show that our NEE estimates are at the upper range of the distribution, but still realistic. Also evapotranspiration estimates, evaluated in the Budyko framework, are in a similar range but with a large inter-annual variability. We identified instrumental problems and variability from different flux partitioning algorithms as a large source of uncertainty, but with only minor influence on the trends found. Warming and rising CO2-concentrations are consistent with the observed trend, but cannot be disentangled from site-specific changes such as the recovery from “Waldsterben” after liming and an increase in heterogeneity after a wind-throw, which likely plays the most important role in the observed dynamics. As such transitions from an “ideal” to a disturbed or heterogeneous site are likely more-often the case at FLUXNET stations built 10–20 years ago, a systematic bias in regional studies can only be avoided by taking each single site history into account.