Temperaturveraenderungen in Bodennaehe bei ploetzlichen Temperaturstuerzen oder Warmlufteinbruechen wirken sich verzoegert auf die Bodentemperatur aus. Es kommt zu Kondensations- bzw. Verdampfungsvorgaengen und damit Reduzierung oder Steigerung der LCKW-Konzentration in der Bodenluft. Entsprechende Zusammenhaenge unter Einbeziehung der Bodenfeuchte werden theoretisch und praktisch untersucht.
Our long term activities aim at a functional understanding of alpine plant life. Overall our research shifted gradually from studying resource acquisition (e.g. photosynthesis) toward resource investment and questions of developement. As with treeline, sink activity seems to be the major determinant of growth. A common misconception associated with alpine plant life finds its expression in the use of the terms 'stress' and 'limitation'. See the critique in: Körner C (1998) Alpine plants: stressed or adapted? In: Press MC, Scholes JD, Barker MG (eds.) Physiological Plant Ecology. Blackwell Science , 297-311. Ongoing experimental work: The influence of photoperiod on growth and development in high elevation taxa (Ph.D. by Franziska Keller in cooperation with the Dept. of Geography, University of Fribourg). We test, whether and which species are responsive to earlier snow melt. It appears there exists a suite of different sensitivities, suggesting biodiversity shifts. We also tested the influence of nutrient addition on high elevation pioneer plants and run a longer term project on the interactive effect on sheep tramplng, nitrogen deposition and warming as part of the Swiss National Project NFP 48. A Europe-wide assessment of ground temperatures in alpine grassland is part of ALPNET (see associated organisations). The assessment provides a basis for comparing biodiversity in alpine biota from 69 to 37 degree of northern latitude. (Nagy et al. (2003) Ecological Studies, Vol. 167. 577 p. Springer, Berlin). A synthesis of research in functional ecology of alpine plants over the past 100 years was published in 1999.
The Tropical Glaciology Group's research on Kilimanjaro started in 2002 and is in progress. Central aspects of our research plan are: 1) Development of the working hypothesis: From a synopsis of (i) proxy data indicating changes in East African climate since ca. 1850, (ii) 20th century instrumental data (temperature and precipitation), and (iii) the observations and interpretations made during two periods of fieldwork (June 2001 and July 2002) a scenario of modern glacier retreat on Kibo is reconstructed. This scenario offers the working hypothesis for our project. 2) Impact of local climate on the glaciers: This goal involves micrometeorological measurements on the glaciers, and the application of collected data to full glacier energy and mass balance models. These models quantify the impact of local climate on a glacier, based on pure physical system knowledge. Our models are validated by measured mass loss and surface temperature. 3) Latest Extent of the Kilimanjaro glaciers: Here, a satellite image was analyzed to derive the surface area and spatial distribution of glaciers on Kilimanjaro in February 2003. To validate this approach, an aerial flight was conducted in July 2005. 4) Linking local climate to large-scale circulation: As glacier behavior on Kilimanjaro, a totally free-standing mountain, is likely to reflect changes in larger-scale climate, this goal explores the large-scale climate mechanisms driving local Kilimanjaro climate. Well known large-scale forcings of east African climate are sea surface temperature variations in the Pacific and, more important, in the Indian Ocean. 5) Regional modification of large-scale circulation: The regional precipitation response in East Africa due to large-scale forcing is not adequately resolved in a global climate model as used in 4). Thus, mesoscale model experiments with the numerical atmospheric model RAMS will be conducted within this goal. They are thought to reveal the modification of atmospheric flow by the Kilimanjaro massif on a regional scale. 6) Practical aspects: Based on micro- and mesoscale results, (i) how much water is provided by glaciers, (ii) providing future projections of glacier behavior as basis for economic and societal studies (practical part), e.g., for studies on the impact of vanishing glaciers on Kibo's touristic appeal, and (iii) which impact does deforestation on the Kilimanjaro slopes have on summit climate? Referring to item 2), two new automatic weather stations have been installed in February 2005. They complete a station operated by Massachusetts University on the surface of the Northern Icefield since 2000.
Das ist eine senseBox der Humboldt Explorers. Weitere Informationen unter www.humboldt-explorers.de
Beobachtungen an deutschlandweit verteilten Straßenwetterstationen. Meteorologische Parameter wie Temperatur, Niederschlag usw. werden alle 15 Minuten gemessen.
The weather station was set up in the beginning of the sampling period in August 2019 and ran the entire sampling period with an interruption between 30th January 2020 and 11th June 2020. Air and soil temperatures, relative humidity and photosynthetic flux density were measured on hourly intervals. Please note that the ground temperature sensor was situated 20 above the ground and therefore the measured medium depends on the conditions of the field site. Before rewetting, the medium was air, but after rewetting, when the area was usually inundated with water it indicates water temperatures.
Das ist eine senseBox der Humboldt Explorers. Weitere Informationen unter: https://www.humboldt-explorers.de/
ICON-EPS 0.5º x 0.5º regular lat/lon grid, up to +180h every 6h, runs 00/12 UTC varios parameter, varios level, varios threshold
Das ist eine senseBox der Humboldt Explorers. Weitere Informationen unter: https://www.humboldt-explorers.de/
Das ist eine senseBox der Humboldt Explorers. https://www.humboldt-explorers.de/
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