22 research outputs found

    Application of a multi-step error filter for postprocessing of atmospheric flux and meteorological basic data

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    Potential of Airborne LiDAR Derived Vegetation Structure for the Prediction of Animal Species Richness at Mount Kilimanjaro

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    The monitoring of species and functional diversity is of increasing relevance for the development of strategies for the conservation and management of biodiversity. Therefore, reliable estimates of the performance of monitoring techniques across taxa become important. Using a unique dataset, this study investigates the potential of airborne LiDAR-derived variables characterizing vegetation structure as predictors for animal species richness at the southern slopes of Mount Kilimanjaro. To disentangle the structural LiDAR information from co-factors related to elevational vegetation zones, LiDAR-based models were compared to the predictive power of elevation models. 17 taxa and 4 feeding guilds were modeled and the standardized study design allowed for a comparison across the assemblages. Results show that most taxa (14) and feeding guilds (3) can be predicted best by elevation with normalized RMSE values but only for three of those taxa and two of those feeding guilds the difference to other models is significant. Generally, modeling performances between different models vary only slightly for each assemblage. For the remaining, structural information at most showed little additional contribution to the performance. In summary, LiDAR observations can be used for animal species prediction. However, the effort and cost of aerial surveys are not always in proportion with the prediction quality, especially when the species distribution follows zonal patterns, and elevation information yields similar results

    remote: Empirical Orthogonal Teleconnections in R

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    In climate science, teleconnection analysis has a long standing history as a means for describing regions that exhibit above average capability of explaining variance over time within a certain spatial domain (e.g., global). The most prominent example of a global coupled ocean-atmosphere teleconnection is the El Nin ?o Southern Oscillation. There are numerous signal decomposition methods for identifying such regions, the most widely used of which are (rotated) empirical orthogonal functions. First introduced by van den Dool, Saha, and Johansson (2000), empirical orthogonal teleconnections (EOT) denote a regression based approach that allows for straight-forward interpretation of the extracted modes. In this paper we present the R implementation of the original algorithm in the remote package. To highlight its usefulness, we provide three examples of potential use- case scenarios for the method including the replication of one of the original examples from van den Dool et al. (2000). Furthermore, we highlight the algorithms use for cross- correlations between two different geographic fields (identifying sea surface temperature drivers for precipitation), as well as statistical downscaling from coarse to fine grids (using Normalized Difference Vegetation Index fields)

    A Comparative Study of Cross-Product NDVI Dynamics in the Kilimanjaro Region—A Matter of Sensor, Degradation Calibration, and Significance

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    While satellite-based monitoring of vegetation activity at the earth’s surface is of vital importance for many eco-climatological applications, the degree of agreement among certain sensors and products providing estimates of the Normalized Difference Vegetation Index (NDVI) has been found to vary considerably. In order to assess the extent of such differences in highly heterogeneous terrain, we analyze and compare intra-annual seasonal fluctuations and long-term monotonic trends (2003–2012) in the Kilimanjaro region, Tanzania. The considered NDVI datasets include the Moderate Resolution Imaging Spectroradiometer (MODIS) products from Terra and Aqua, Collections 5 and 6, and the 3rd Generation Global Inventory Modeling and Mapping Studies (GIMMS) product. The degree of agreement in seasonal fluctuations is assessed by calculating a pairwise Index of Association (IOAs), whereas long-term trends are derived from the trend-free pre-whitened Mann–Kendall test. On the seasonal scale, the two Terra-MODIS products (and, accordingly, the two Aqua-MODIS products) are best associated with each other, indicating that the seasonal signal remained largely unaffected by the new Collection 6 calibration approach. On the long-term scale, we find that the negative impacts of band ageing on Terra-MODIS NDVI have been accounted for in Collection 6, which now distinctly outweighs Aqua-MODIS in terms of greening trends. GIMMS NDVI, by contrast, fails to capture small-scale seasonal and trend patterns that are characteristic for the highly fragmented landscape which is likely owing to the coarse spatial resolution. As a short digression, we also demonstrate that the amount of false discoveries in the determined trend fraction is distinctly higher for p < 0.05 ( 52.6 % ) than for p < 0.001 ( 2.2 % ) which should point the way for any future studies focusing on the reliable deduction of long-term monotonic trends

    Hourly gridded air temperatures of South Africa derived from MSG SEVIRI (2010-2014), links to files

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    This dataset consists of hourly gridded 3.5x3.5 km air temperature data for entire South Africa. The data set was created using a Random Forest approach: MSG SEVIRI data from 2010 to 2014 were used and related to air temperature measured by 78 weather stations. An external validation on new climate stations and years that were not used for model training indicated the ability of the model to predict air temperature with a RMSE of 2.61°C and a RÂČ of 0.89. The data set hence allows for spatio-temporal pattern analysis as well as for the detection of trends which is relevant in the context of climate change. The data are available as one geotif per day in geos projection (proj4String: +proj=geos +lon_0=0 +h=35785831 +x_0=0 +y_0=0 +ellps=WGS84 +units=m +no_defs ). Note that the unit of the data is °C*10

    Development of 3D Biofabricated Cell Laden Hydrogel Vessels and a Low‐Cost Desktop Printed Perfusion Chamber for In Vitro Vessel Maturation

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    Abstract The vascular system represents the key supply chain for nutrients and oxygen inside the human body. Engineered solutions to produce sophisticated alternatives for autologous or artificial vascular implants to sustainably replace diseased vascular tissue still remain a key challenge in tissue engineering. In this paper, cell‐laden 3D bioplotted hydrogel vessel‐like constructs made from alginate di‐aldehyde (ADA) and gelatin (GEL) are presented. The aim is to increase the mechanical stability of fibroblast‐laden ADA‐GEL vessels, tailoring them for maturation under dynamic cell culture conditions. BaCl2 is investigated as a crosslinker for the oxidized alginate‐gelatin system. Normal human dermal fibroblast (NHDF)‐laden vessel constructs are optimized successfully in terms of higher stiffness by increasing ADA concentration and using BaCl2, with no toxic effects observed on NHDF. Contrarily, BaCl2 crosslinking of ADA‐GEL accelerates cell attachment, viability, and growth from 7d to 24h compared to CaCl2. Moreover, alignment of cells in the longitudinal direction of the hydrogel vessels when extruding the cell‐laden hydrogel crosslinked with Ba2+ is observed. It is possible to tune the stiffness of ADA‐GEL by utilizing Ba2+ as crosslinker. In addition, a customized, low‐cost 3D printed polycarbonate (PC) perfusion chamber for perfusion of vessel‐like constructs is introduced

    Seasonal and long-term vegetation dynamics from 1-km GIMMS-based NDVI time series at Mt. Kilimanjaro, Tanzania

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    This dataset consists of GeoTIFF fille for GIMMS NDVI downscaled record (1982–2011) that was resampled from 8 km to 1 km spatial resolution

    Raw climate station data for the southern slopes of Kilimanjaro, Tanzania

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    The climate station network was set up on the southern slopes of Kilimanjaro, Tanzania, in 2010 and presents the recorded characteristics of air temperature, air humidity, and precipitation from both a plot-based and area-wide perspectives. The station set-up followed a hierarchical approach covering an elevation as well as a land-use disturbance gradient. It consisted of 52 basic stations measuring ambient air temperature and above-ground air humidity and 11 precipitation measurement sites, with recording intervals of 5 min. With respect to precipitation observations, the network extended the long-term recordings of A. Hemp which has installed and maintained up to 117 multi-month accumulating rainfall buckets in the region since 1997

    Monthly maps of air temperature and air humidity of the southern slopes of Kilimanjaro, Tanzania

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    Monthly maps of air temperature and air humidity of the southern slopes of Kilimanjaro, Tanzania. The dataset is part of our study on eco‐meteorological characteristics of the southern slopes of Kilimanjaro, Tanzania ([https://doi.org/10.1002/joc.4552]). (1) ta200_kriging.zip The dataset contains interpolate monthly air temperature maps using universal kriging with elevation, aspect, slope, sky‐view factor and mean monthly normalized difference vegetation index (NDVI) as external drift variables. This corresponds to step 5 in chapter 3.1 of [https://doi.org/10.1002/joc.4552]. (2) rh200_kriging.zip The dataset contains interpolate monthly air humidity maps using universal kriging with elevation, aspect, slope, sky‐view factor and mean monthly normalized difference vegetation index (NDVI) as external drift variables. This corresponds to step 5 in chapter 3.1 of [https://doi.org/10.1002/joc.4552]. (3) ta200_kriging_multi-year_average.zip and rh200_kriging_multi-year_average.zip The dataset contains multi-year monthly averages from (1) and (2) and a map of the multi-year annual mean air temperature and humidity. This corresponds to step 6 in chapter 3.1 of [https://doi.org/10.1002/joc.4552]. For the datasets (1) and (2), we used 5-min measurements between 2011 and 2014 of 52 climate stations that distributed across the southern slopes of Mt. Kilimanjaro. We aggregated the 5-min measurements to hourly observations and filled existing gaps of up to 1 year through multivariate regression using the five nearest stations. We aggregated the gap-filled hourly data to daily averages if at least 22 h of valid records exist for that day at a specific station. Finally, we aggregated the daily averages to monthly averages if a single month has at least 20 valid daily records
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