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Die vorliegende Arbeit wurde auf der Grundlage begutachteter Publikationen als kumulative Dissertation verfasst. Ziel war hier, das zeitliche Spektrum des Niederschlages unter sich bereits geänderten und zukünftig möglichen Klimabedingungen zu untersuchen, um daraus risikobehaftete Auswirkungen auf den Wasserhaushalt ableiten zu können. Ausgehend von den für Sachsen bzw. Mitteldeutschland jahreszeitlich berechneten Trends für den Niederschlag im Zeitraum 1951-2000 wurde hier der Schwerpunkt auf das Verhalten des Starkniederschlages im Einzugsgebiet der Weißeritz (Osterzgebirge) während der Vegetationsperiode gesetzt. Unter Verwendung von Extremwertverteilungen wurde das lokale Starkniederschlagsgeschehen im Referenzzeitraum 1961-2000 für Ereignisandauern von 1-24 Stunden und deren Wiederkehrzeiten von 5-100 Jahren aus statistischer Sicht beschrieben. Mittels eines wetterlagenbasierten statistischen Downscaling wurden mögliche Änderungen im Niveau des zeitlich höher aufgelösten Niederschlagspektrums gegenüber dem Referenzspektrum auf die Zeitscheiben um 2025 (2011-2040) und 2050 (2036-2065) projiziert. Hierfür wurden die zu erwartenden Klimabedingungen für das IPCC-Emissionsszenario A1B angenommen. Mittels eines problemangepassten Regionalisierungsalgorithmus´ konnte eine Transformation der Punktinformationen in eine stetige Flächeninformation erreicht werden. Dabei wurden verteilungsrelevante Orografieeffekte auf den Niederschlag maßstabsgerecht berücksichtigt. Die signifikanten Niederschlagsabnahmen im Sommer bzw. in der Vegetationsperiode sind in Sachsen mit einer Zunahme und Intensivierung von Starkniederschlägen kombiniert. Hieraus entsteht ein Konfliktpotenzial zwischen Hochwasserschutz auf der einen und (Trink-) Wasserversorgung auf der anderen Seite. Für die zu erwartenden Klimabedingungen der Zeitscheiben um 2025 und 2050 wurden für das Einzugsgebiet der Weißeritz zunehmend positive, nicht-lineare Niveauverschiebungen im zeitlich höher aufgelösten Spektrum des Starkniederschlages berechnet. Für gleich bleibende Wiederkehrzeiten ergaben sich größere Regenhöhen bzw. für konstant gehaltene Regenhöhen kleinere Wiederkehrzeiten. Aus dem erhaltenen Änderungssignal kann gefolgert werden, dass der sich fortsetzende allgemeine Erwärmungstrend mit einer Intensivierung des primär thermisch induzierten, konvektiven Starkniederschlagsgeschehens einhergeht, was in Sachsen mit einem zunehmend häufigeren Auftreten von Starkregenereignissen kürzerer Andauer sowie mit einer zusätzlichen orografischen Verstärkung von Ereignissen längerer Andauer verbunden ist. Anhand des Klimaquotienten nach Ellenberg wurden Effekte des rezenten Klimatrends auf die Verteilung der potenziellen natürlichen Vegetation in Mitteldeutschland beispielhaft untersucht. Über eine Korrektur der Berechnungsvorschrift konnte eine Berücksichtigung der trendbehafteten klimatologischen Rahmenbedingungen, insbesondere dem negativen Niederschlagstrend im Sommer, erreicht werden. Insgesamt konnte festgestellt werden, dass die regionalen Auswirkungen des globalen Klimawandels massive Änderungen in der raum-zeitlichen Struktur des Niederschlages in Sachsen zur Folge haben, was unvermeidlich eine komplexe Wirkungskette auf den regionalen Wasserhaushalt zur Folge hat und mit Risiken verbunden ist. / This paper was written as a cumulative doctoral thesis based on appraised publications. Its objective was to study the temporal spectrum of precipitation under already changed or possible future climate conditions in order to derive effects on the water budget which are fraught with risks. Based on seasonal trends as established for Saxony and Central Germany for precipitation in the period of 1951-2000, the focus was on the behaviour of heavy precipitation in the catchment area of the Weißeritz (eastern Ore Mountains) during the growing season. Using distributions of extreme values, the local heavy precipitation behaviour in the reference period of 1961-2000 was described from a statistical point of view for event durations of 1-24 hours and their return periods of 5-100 years. Statistical downscaling based on weather patterns was used to project possible changes in the level of the high temporal resolution spectrum of precipitation, compared with the reference spectrum, to the time slices around 2025 (2011-2040) and 2050 (2036-2065). The IPCC A1B emission scenario was assumed for expected climate conditions for this purpose. Using a regionalisation algorithm adapted to the problem made it possible to achieve a transformation of local information into areal information. In doing so, distribution-relevant orographic effects on precipitation were taken into consideration in a manner true to scale. Significant decreases in precipitation in summer and during the growing season are combined with an increase and intensification of heavy precipitation in Saxony. This gives rise to a potential for conflict between the need for flood protection, on the one hand, and the supply of (drinking) water, on the other hand. For the expected climate conditions of the time slices around 2025 and 2050, increasingly positive, non-linear shifts in the level of the high temporal resolution spectrum of heavy precipitation were calculated for the catchment of the Weißeritz. Higher amounts of rain were found if the return periods were kept constant, and shorter return periods were found if the rain amounts were kept constant. It may be concluded from the change signal obtained that the continuing general warming trend is accompanied by an intensification of the primarily thermally induced convective behaviour of heavy precipitation. In Saxony, this is associated with an increasingly frequent occurrence of heavy precipitation events of short duration and with an additional orographic intensification of events of long duration. Using the Ellenberg climate quotient, effects of the recent climate trend on the distribution of potential natural vegetation in Central Germany were studied by way of example. Underlying climatological conditions subject to a trend, in particular the negative trend of precipitation in summer, were taken into consideration by a modification of the calculation rule. All in all, it was found that regional effects of global climate change bring about massive changes in the spatiotemporal structure of precipitation in Saxony, which inevitably leads to a complex chain of impact on the regional water budget and is fraught with risks.

The issue of rapid change in environmental conditions under which ecosystem processes and human interventions will take place in the future is relatively new to forestry, whereas the provision of ecosystem services, e.g., timber or fresh water, is at the very heart of the original concept of forest management. Forest managers have developed ambitious deterministic approaches to provide the services demanded, and thus the use of deterministic approaches for adapting to climate change seem to be a logical continuation. However, as uncertainty about the intensity of climate change is high, forest managers need to answer this uncertainty conceptually. One may envision an indeterministic approach to cope with this uncertainty; but how the services will be provided in such a concept remains unclear. This article aims to explore the fundamental aspects of both deterministic and indeterministic approaches used in forestry to cope with climate change, and thereby point out trade-offs in service provisioning and adaptability. A forest owner needs to be able to anticipate these trade-offs in order to make decisions towards sustainable forest management under climate change.

Die vorliegende Arbeit wurde auf der Grundlage begutachteter Publikationen als kumulative Dissertation verfasst. Ziel war hier, das zeitliche Spektrum des Niederschlages unter sich bereits geänderten und zukünftig möglichen Klimabedingungen zu untersuchen, um daraus risikobehaftete Auswirkungen auf den Wasserhaushalt ableiten zu können. Ausgehend von den für Sachsen bzw. Mitteldeutschland jahreszeitlich berechneten Trends für den Niederschlag im Zeitraum 1951-2000 wurde hier der Schwerpunkt auf das Verhalten des Starkniederschlages im Einzugsgebiet der Weißeritz (Osterzgebirge) während der Vegetationsperiode gesetzt. Unter Verwendung von Extremwertverteilungen wurde das lokale Starkniederschlagsgeschehen im Referenzzeitraum 1961-2000 für Ereignisandauern von 1-24 Stunden und deren Wiederkehrzeiten von 5-100 Jahren aus statistischer Sicht beschrieben. Mittels eines wetterlagenbasierten statistischen Downscaling wurden mögliche Änderungen im Niveau des zeitlich höher aufgelösten Niederschlagspektrums gegenüber dem Referenzspektrum auf die Zeitscheiben um 2025 (2011-2040) und 2050 (2036-2065) projiziert. Hierfür wurden die zu erwartenden Klimabedingungen für das IPCC-Emissionsszenario A1B angenommen. Mittels eines problemangepassten Regionalisierungsalgorithmus´ konnte eine Transformation der Punktinformationen in eine stetige Flächeninformation erreicht werden. Dabei wurden verteilungsrelevante Orografieeffekte auf den Niederschlag maßstabsgerecht berücksichtigt. Die signifikanten Niederschlagsabnahmen im Sommer bzw. in der Vegetationsperiode sind in Sachsen mit einer Zunahme und Intensivierung von Starkniederschlägen kombiniert. Hieraus entsteht ein Konfliktpotenzial zwischen Hochwasserschutz auf der einen und (Trink-) Wasserversorgung auf der anderen Seite. Für die zu erwartenden Klimabedingungen der Zeitscheiben um 2025 und 2050 wurden für das Einzugsgebiet der Weißeritz zunehmend positive, nicht-lineare Niveauverschiebungen im zeitlich höher aufgelösten Spektrum des Starkniederschlages berechnet. Für gleich bleibende Wiederkehrzeiten ergaben sich größere Regenhöhen bzw. für konstant gehaltene Regenhöhen kleinere Wiederkehrzeiten. Aus dem erhaltenen Änderungssignal kann gefolgert werden, dass der sich fortsetzende allgemeine Erwärmungstrend mit einer Intensivierung des primär thermisch induzierten, konvektiven Starkniederschlagsgeschehens einhergeht, was in Sachsen mit einem zunehmend häufigeren Auftreten von Starkregenereignissen kürzerer Andauer sowie mit einer zusätzlichen orografischen Verstärkung von Ereignissen längerer Andauer verbunden ist. Anhand des Klimaquotienten nach Ellenberg wurden Effekte des rezenten Klimatrends auf die Verteilung der potenziellen natürlichen Vegetation in Mitteldeutschland beispielhaft untersucht. Über eine Korrektur der Berechnungsvorschrift konnte eine Berücksichtigung der trendbehafteten klimatologischen Rahmenbedingungen, insbesondere dem negativen Niederschlagstrend im Sommer, erreicht werden. Insgesamt konnte festgestellt werden, dass die regionalen Auswirkungen des globalen Klimawandels massive Änderungen in der raum-zeitlichen Struktur des Niederschlages in Sachsen zur Folge haben, was unvermeidlich eine komplexe Wirkungskette auf den regionalen Wasserhaushalt zur Folge hat und mit Risiken verbunden ist. / This paper was written as a cumulative doctoral thesis based on appraised publications. Its objective was to study the temporal spectrum of precipitation under already changed or possible future climate conditions in order to derive effects on the water budget which are fraught with risks. Based on seasonal trends as established for Saxony and Central Germany for precipitation in the period of 1951-2000, the focus was on the behaviour of heavy precipitation in the catchment area of the Weißeritz (eastern Ore Mountains) during the growing season. Using distributions of extreme values, the local heavy precipitation behaviour in the reference period of 1961-2000 was described from a statistical point of view for event durations of 1-24 hours and their return periods of 5-100 years. Statistical downscaling based on weather patterns was used to project possible changes in the level of the high temporal resolution spectrum of precipitation, compared with the reference spectrum, to the time slices around 2025 (2011-2040) and 2050 (2036-2065). The IPCC A1B emission scenario was assumed for expected climate conditions for this purpose. Using a regionalisation algorithm adapted to the problem made it possible to achieve a transformation of local information into areal information. In doing so, distribution-relevant orographic effects on precipitation were taken into consideration in a manner true to scale. Significant decreases in precipitation in summer and during the growing season are combined with an increase and intensification of heavy precipitation in Saxony. This gives rise to a potential for conflict between the need for flood protection, on the one hand, and the supply of (drinking) water, on the other hand. For the expected climate conditions of the time slices around 2025 and 2050, increasingly positive, non-linear shifts in the level of the high temporal resolution spectrum of heavy precipitation were calculated for the catchment of the Weißeritz. Higher amounts of rain were found if the return periods were kept constant, and shorter return periods were found if the rain amounts were kept constant. It may be concluded from the change signal obtained that the continuing general warming trend is accompanied by an intensification of the primarily thermally induced convective behaviour of heavy precipitation. In Saxony, this is associated with an increasingly frequent occurrence of heavy precipitation events of short duration and with an additional orographic intensification of events of long duration. Using the Ellenberg climate quotient, effects of the recent climate trend on the distribution of potential natural vegetation in Central Germany were studied by way of example. Underlying climatological conditions subject to a trend, in particular the negative trend of precipitation in summer, were taken into consideration by a modification of the calculation rule. All in all, it was found that regional effects of global climate change bring about massive changes in the spatiotemporal structure of precipitation in Saxony, which inevitably leads to a complex chain of impact on the regional water budget and is fraught with risks.

The desire for local governments to adapt to climate change seems logically relevant as weather extremes inhibit the ability of local governments to protect public health and safety and to ensure delivery of public services. By conducting planned adaptation to climate change local governments enable themselves to minimize risk and increase adaptive capacity to deal with climate change impacts. In the midst of a federal government, minus the Obama administration, that has tended to downplay the importance of climate change, action by local level governments - cities in particular - in the U.S. have been at the forefront of action on climate change. Little attention has been given to local government adaptation in rural areas by both researchers and policy makers alike. Rural areas are at risk to changes in climate because they tend to be reliant on climate sensitive industries, comprised of vulnerable populations, such as the elderly and very young and to possess few resources to conduct land-use and other planning. This dissertation expands upon previous research by examining the decision to conduct planned adaptation by both urban and rural local government adaptation to climate change (RQ1) and by identifying the influences on the decision of local governments in both urban and rural areas to conduct planned adaptation to climate change (RQ2). New York State was selected as an appropriate case study to answer research questions because of the drastic contrast between urban and rural areas of the state. On the one hand, it has been one of the most progressive states in terms of climate change policy including its largest local government New York City; on the other hand, it is comprised of many rural local governments suffering from population and economic decline. An online survey was distributed to all New York State local governments in November/December 2011 and supplemented by informant discussions conducted before and after the survey. While a considerable amount of time has passed since the survey was conducted, it took place during what appears to be a particular timeframe in political history where the U.S. president supported action on climate change. Results of this study show strong differences in resource availability and the likelihood of urban vs. rural elected officials to conduct planned adaptation. One hundred and forty-two responses were received from large and small cities, towns, villages and counties. A traditional deductive research design was deployed to answer research questions. To examine the influences on the decision of local elected officials to conduct planned adaptation hypotheses were developed based on previous empirical studies and Mohr’s 1969 hypothesis that “Innovation is related to the motivation to innovate, inversely related to the strength of obstacles to innovation, and directly related to the availability of resources for overcoming such obstacles” (Mohr, 1969, p. 111). Two dependent variables were measured (1) planned adaptation or conscious decisions to adapt to climate change and an alternate dependent variable (2) formal and informal discussion of climate change within the local government. Independent variables measured related to local elected official motivation to conduct planned adaptation in the form of climate weather related concerns in New York State (i.e. extreme weather, water quality, and ecological changes), resource availability within the local government (i.e. budget, staff, climate change expertise) and the existence of obstacles toward planned adaptation external to local governments (i.e. public support, federal and state informational and financial support). The results of the survey showed that a small minority of local governments in New York State had decided to conduct planned adaptation to climate change. Over half of the sample was identified as conducting some form of spontaneous or reactive adaptation which consisted mostly of actions to minimize flood risk (i.e. update storm-water infrastructure, manage flood plains, promote open space). However, no local government surveyed had been identified as having successfully implemented an adaptation plan. Informal discussions were found to be occurring among half of the sample surveyed with a small number of local governments discussing climate change formally. According to informant discussions, the low level of planned adaptation among New York State local governments can be explained by a number of factors including a non-requirement to conduct planned adaptation, varying policy, resource and incentive conditions throughout the state, a lack of urgency to adapt to climate change and, finally, the absence of a support system to conduct planned adaptation. Results of hypothesis testing indicate that local governments are more likely to conduct planned adaptation to climate change where: A) climate change concerns are water related, B) budget, staff and climate change expertise are available and C) public support to address climate change impacts as well as state and federal informational support are available. Financial support from state and federal governments did not appear to influence the decision to conduct planned adaptation. Rural local governments were found less likely than urban local governments to be discussing climate change and to be conducting planned adaptation which is likely to be related to organizational size and the availability of resources to conduct planned adaptation measures. This dissertation contributes to understanding how local governments are adapting to climate change in New York State, what influences the decision of elected officials to conduct planned adaptation to climate change and how experiences may differ from municipality type — especially related to urban vs. rural local governments.

The issue of rapid change in environmental conditions under which ecosystem processes and human interventions will take place in the future is relatively new to forestry, whereas the provision of ecosystem services, e.g., timber or fresh water, is at the very heart of the original concept of forest management. Forest managers have developed ambitious deterministic approaches to provide the services demanded, and thus the use of deterministic approaches for adapting to climate change seem to be a logical continuation. However, as uncertainty about the intensity of climate change is high, forest managers need to answer this uncertainty conceptually. One may envision an indeterministic approach to cope with this uncertainty; but how the services will be provided in such a concept remains unclear. This article aims to explore the fundamental aspects of both deterministic and indeterministic approaches used in forestry to cope with climate change, and thereby point out trade-offs in service provisioning and adaptability. A forest owner needs to be able to anticipate these trade-offs in order to make decisions towards sustainable forest management under climate change.