Modeling of deep-convective

Deep convection by pyro-cumulonimbus clouds (pyroCb) can transport large amounts of forest fire smoke into the upper troposphere and lower stratosphere. Here, results from numerical simulations of such deep convective smoke transport are presented. The structure, shape and injection height of the pyroCb simulated for a specific case study are in good agreement with observations. The model results confirm that substantial amounts of smoke are injected into the lower stratosphere. Small-scale mixing processes at the cloud top result in a significant enhancement of smoke injection into the stratosphere. Sensitivity studies show that the release of sensible heat by the fire plays an important role for the dynamics of the pyroCb. Furthermore, the convection is found to be very sensitive to background meteorological conditions. While the abundance of aerosol particles acting as cloud condensation nuclei (CCN) has a strong influence on the microphysical structure of the pyroCb, the CCN effect on the convective dynamics is rather weak. The release of latent heat dominates the overall energy budget of the pyroCb. Since most of the cloud water originates from moisture entrained from the background atmosphere, the fire-released moisture contributes only minor to convection dynamics. Sufficient fire heating, favorable meteorological conditions, and small-scale mixing processes at the cloud top are identified as the key ingredients for troposphere-to-stratosphere transport by pyroCb convection.

Waldbrandprognose und Waldbrandbekämpfung in Deutschland

Ist Deutschland auf Waldbrandkatastrophen vorbereitet? Dies ist die zentrale Frage dieser wissenschaftlichen Arbeit. Zahlreiche Großwaldbrände der Vergangenheit zeigen ein deutliches Waldbrandpotential für die bundesdeutschen Areale, speziell in Ostdeutschland. Als eine der Folgen des global warming ist zukünftig mit einem Anstieg der Gefahrensituation zu rechnen. Anhand der Untersuchung zweier Katastrophenwaldbrände wurden Schwachstellen bei der Bekämpfung dieser Waldbrände aufgezeigt, aber auch positive Aspekte herausgestellt. Die wichtigste Erkenntnis ist hierbei die große Bedeutung der Brandbekämpfung aus der Luft. Sie spielt die Schlüsselrolle bei der Bekämpfung von Großwaldbränden. Daher untersucht diese Arbeit die aktuelle Situation in Deutschland und erstellt erstmals ein bundesweites Kataster der Hubschrauberaußenlastbehälter sowie den dazugehörigen Trägerfahrzeugen (Hubschrauber). Aufgrund dieses Katasters sowie einer Auflistung der Systeme zur Branddetektion (Feuerwachtürme und kameragestützte Systeme) kommt diese Arbeit zu dem Ergebnis, dass man in Deutschland gut auf Waldbrandkatastrophen vorbereitet ist. Gleichzeitig liefert diese Arbeit aber auch Optimierungsmöglichkeiten in Form eines Maßnahmenkatalogs. So ist beispielsweise das System der Waldbrandprognose nach M-68 zu überarbeiten, da es die tatsächliche Gefährdungslage teilweise unterschätzt, Simulationsprogramme zur Ausbreitung von Waldbränden sind zu entwickeln, Sicherheitsregeln sind einzuführen. Weiterhin ist die indirekte Brandbekämpfung durch die Aufstellung von task-forces in Deutschland erstmalig zu ermöglichen.

External drivers of biogeochemical cycles in a tropical montane forest in Ecuador

Successful conservation of tropical montane forest, one of the most threatened ecosystems on earth, requires detailed knowledge of its biogeochemistry. Of particular interest is the response of the biogeochemical element cycles to external influences such as element deposition or climate change. Therefore the overall objective of my study was to contribute to improved understanding of role and functioning of the Andean tropical montane forest. In detail, my objectives were to determine (1) the role of long-range transported aerosols and their transport mechanisms, and (2) the role of short-term extreme climatic events for the element budget of Andean tropical forest. In a whole-catchment approach including three 8-13 ha microcatchments under tropical montane forest on the east-exposed slope of the eastern cordillera in the south Ecuadorian Andes at 1850-2200 m above sea level I monitored at least in weekly resolution the concentrations and fluxes of Ca, Mg, Na, K, NO3-N, NH4-N, DON, P, S, TOC, Mn, and Al in bulk deposition, throughfall, litter leachate, soil solution at the 0.15 and 0.3 m depths, and runoff between May 1998 and April 2003. I also used meteorological data from my study area collected by cooperating researchers and the Brazilian meteorological service (INPE), as well as remote sensing products of the North American and European space agencies NASA and ESA. My results show that (1) there was a strong interannual variation in deposition of Ca [4.4-29 kg ha-1 a-1], Mg [1.6-12], and K [9.8-30]) between 1998 and 2003. High deposition changed the Ca and Mg budgets of the catchments from loss to retention, suggesting that the additionally available Ca and Mg was used by the ecosystem. Increased base metal deposition was related to dust outbursts of the Sahara and an Amazonian precipitation pattern with trans-regional dry spells allowing for dust transport to the Andes. The increased base metal deposition coincided with a strong La Niña event in 1999/2000. There were also significantly elevated H+, N, and Mn depositions during the annual biomass burning period in the Amazon basin. Elevated H+ deposition during the biomass burning period caused elevated base metal loss from the canopy and the organic horizon and deteriorated already low base metal supply of the vegetation. Nitrogen was only retained during biomass burning but not during non-fire conditions when deposition was much smaller. Therefore biomass burning-related aerosol emissions in Amazonia seem large enough to substantially increase element deposition at the western rim of Amazonia. Particularly the related increase of acid deposition impoverishes already base-metal scarce ecosystems. As biomass burning is most intense during El Niño situations, a shortened ENSO cycle because of global warming likely enhances the acid deposition at my study forest. (2) Storm events causing near-surface water flow through C- and nutrient-rich topsoil during rainstorms were the major export pathway for C, N, Al, and Mn (contributing >50% to the total export of these elements). Near-surface flow also accounted for one third of total base metal export. This demonstrates that storm-event related near-surface flow markedly affects the cycling of many nutrients in steep tropical montane forests. Changes in the rainfall regime possibly associated with global climate change will therefore also change element export from the study forest. Element budgets of Andean tropical montane rain forest proved to be markedly affected by long-range transport of Saharan dust, biomass burning-related aerosols, or strong rainfalls during storm events. Thus, increased acid and nutrient deposition and the global climate change probably drive the tropical montane forest to another state with unknown consequences for its functions and biological diversity.