Einfluss der Flächenwahl, Anbaudichte und Landschaftsstruktur auf den Befallsstatus und die Ausbreitung der Möhrenfliege Psila rosae F. (Diptera: Psilidae) im ökologischen Möhrenanbau

Durch die vermehrte Nachfrage von Biomöhren im Lebensmitteleinzelhandel ist die Anbaufläche ökologisch erzeugter Möhren in den letzten zehn Jahren deutlich angestiegen. Der Anbau konzentriert sich auf bestimmte Regionen und erfolgte damit zunehmend auf großen Schlägen in enger räumlicher und zeitlicher Abfolge. Mit der steigenden Wirtspflanzenpräsenz steigt auch der Befallsdruck durch die Möhrenfliege. Während der Schädling im konventionellen Anbau mit Insektiziden kontrolliert wird, stehen dem Ökologischen Landbau bisher keine direkten Regulative zur Verfügung. Ziel der Untersuchungen war es, unter den Praxisbedingungen des ökologischen Möhrenanbaus einzelbetriebliche und überregionale Muster beteiligter Risikofaktoren im Befallsgeschehen zu identifizieren und so Möglichkeiten einer verbesserten Prävention und Regulation aufzuzeigen. Über einen Zeitraum von drei Jahren wurden auf fünf Betrieben in Niedersachsen und Hessen umfangreiche Felddaten erhoben und diese unter Verwendung von GIS – Software und dem Simulationsmodell SWAT analysiert. Untersuchte Einflussgrößen umfassten (1) die Distanz zu vorjährigen Möhrenfeldern, (2) die zeitliche Möhrenanbauperiode, (3) Vegetationselemente und (4) der experimentelle Einsatz von Fangpflanzen zur Unterdrückung der Fliegenentwicklung. Unter der Berücksichtigung deutlicher einzelbetrieblicher Unterschiede sind die wichtigsten Ergebnisse der Studie wie folgt zu benennen: (1) Auf Betrieben mit Befall im zurückliegenden Anbaujahr zeigte sich die Distanz zu vorjährigen Möhrenfeldern als der wichtigste Risikofaktor. Das Ausbreitungsverhalten der 1. Generation Möhrenfliege erwies sich zudem als situationsgebunden anpassungsfähig. Fliegensumme und Befall waren jeweils in dem zu Vorjahresflächen nächstgelegen Feld am größten, während jeweils dahinter liegende Möhrenschläge entsprechend weniger Fliegenzahlen und Befall auswiesen. Aus den Ergebnissen wird als vorrangige Verbreitungskapazität der 1. Generation Möhrenfliegen innerhalb von 1000 m abgeleitet. (2) Betriebe mit kontinuierlicher Möhren - Anbaubauperiode (ca. April – Oktober), die langfristig die Entwicklung sowohl der 1. als auch der 2. Generation Fliegen unterstützten, verzeichneten stärkere Fliegenprobleme. Hinsichtlich einer verbesserten Prävention wird empfohlen mit einer strikten räumlichen Trennung früher und später Sätze ein Aufschaukeln zwischen den Generationen zu vermeiden. (3) Der Einfluss der Vegetation ließ sich weniger eindeutig interpretieren. Einzelbetriebliche Hinweise, dass Kleingehölze (Hecken und Bäume) im Radius zwischen aktueller und vorjähriger Möhrenfläche die Befallswahrscheinlichkeit erhöhen, konnten mit einem berechneten Gesamtmaß für die regionale holzige Vegetation nicht bestätigt werden. Der großräumigen holzigen Vegetation wird im Vergleich zur Feldrandvegetation daher beim Befallsgeschehen eine geringe Bedeutung zugeschrieben. (4) Drei Meter (vier Dämme) breiter Möhren – Fangstreifen auf den vorjährigen Möhrenfeldern eignen sich bereits ab dem Keimblattstadium, um erhebliches Befallspotential zu binden. Eine mechanische Entfernung der Fangpflanzen (Grubbern) mitsamt dem Befallspotential erzielte in 2008 eine 100 %-ige Unterdrückung der Möhrenfliegenentwicklung, in 2009 jedoch nur zu maximal 41 %. Als mögliche Synthese der Ergebnisse zur Ausbreitung der Möhrenfliegen im Frühjahr und zur zeitlichen Koinzidenz mit der Möhrenentwicklung wird als Empfehlung diskutiert, mit Hilfe einer angepassten Flächenwahl die Fliegenausbreitung räumlich an frühen Sätzen zu binden, um entsprechend befallsarme Regionen für entfernt liegende späte (empfindlichere) Möhrensätze zu schaffen.

Downscaling and Modeling the Effects of Climate Change on Hydrology and Water Resources in the Upper Blue Nile River Basin, Ethiopia

The Upper Blue Nile River Basin (UBNRB) located in the western part of Ethiopia, between 7° 45’ and 12° 45’N and 34° 05’ and 39° 45’E has a total area of 174962 km2 . More than 80% of the population in the basin is engaged in agricultural activities. Because of the particularly dry climate in the basin, likewise to most other regions of Ethiopia, the agricultural productivity depends to a very large extent on the occurrence of the seasonal rains. This situation makes agriculture highly vulnerable to the impact of potential climate hazards which are about to inflict Africa as a whole and Ethiopia in particular. To analyze these possible impacts of future climate change on the water resources in the UBNRB, in the first part of the thesis climate projection for precipitation, minimum and maximum temperatures in the basin, using downscaled predictors from three GCMs (ECHAM5, GFDL21 and CSIRO-MK3) under SRES scenarios A1B and A2 have been carried out. The two statistical downscaling models used are SDSM and LARS-WG, whereby SDSM is used to downscale ECHAM5-predictors alone and LARS-WG is applied in both mono-model mode with predictors from ECHAM5 and in multi-model mode with combined predictors from ECHAM5, GFDL21 and CSIRO-MK3. For the calibration/validation of the downscaled models, observed as well as NCEP climate data in the 1970 - 2000 reference period is used. The future projections are made for two time periods; 2046-2065 (2050s) and 2081-2100 (2090s). For the 2050s future time period the downscaled climate predictions indicate rise of 0.6°C to 2.7°C for the seasonal maximum temperatures Tmax, and of 0.5°C to 2.44°C for the minimum temperatures Tmin. Similarly, during the 2090s the seasonal Tmax increases by 0.9°C to 4.63°C and Tmin by 1°C to 4.6°C, whereby these increases are generally higher for the A2 than for the A1B scenario. For most sub-basins of the UBNRB, the predicted changes of Tmin are larger than those of Tmax. Meanwhile, for the precipitation, both downscaling tools predict large changes which, depending on the GCM employed, are such that the spring and summer seasons will be experiencing decreases between -36% to 1% and the autumn and winter seasons an increase of -8% to 126% for the two future time periods, regardless of the SRES scenario used. In the second part of the thesis the semi-distributed, physically based hydrologic model, SWAT (Soil Water Assessment Tool), is used to evaluate the impacts of the above-predicted future climate change on the hydrology and water resources of the UBNRB. Hereby the downscaled future predictors are used as input in the SWAT model to predict streamflow of the Upper Blue Nile as well as other relevant water resources parameter in the basin. Calibration and validation of the streamflow model is done again on 1970-2000 measured discharge at the outlet gage station Eldiem, whereby the most sensitive out the numerous “tuneable” calibration parameters in SWAT have been selected by means of a sophisticated sensitivity analysis. Consequently, a good calibration/validation model performance with a high NSE-coefficient of 0.89 is obtained. The results of the future simulations of streamflow in the basin, using both SDSM- and LARS-WG downscaled output in SWAT reveal a decline of -10% to -61% of the future Blue Nile streamflow, And, expectedly, these obviously adverse effects on the future UBNRB-water availibiliy are more exacerbated for the 2090’s than for the 2050’s, regardless of the SRES.

The prediction of seasonal and inter-annual climate variations and their impacts on the water resources in the eastern seaboard of Thailand

The research of this thesis dissertation covers developments and applications of short-and long-term climate predictions. The short-term prediction emphasizes monthly and seasonal climate, i.e. forecasting from up to the next month over a season to up to a year or so. The long-term predictions pertain to the analysis of inter-annual- and decadal climate variations over the whole 21st century. These two climate prediction methods are validated and applied in the study area, namely, Khlong Yai (KY) water basin located in the eastern seaboard of Thailand which is a major industrial zone of the country and which has been suffering from severe drought and water shortage in recent years. Since water resources are essential for the further industrial development in this region, a thorough analysis of the potential climate change with its subsequent impact on the water supply in the area is at the heart of this thesis research. The short-term forecast of the next-season climate, such as temperatures and rainfall, offers a potential general guideline for water management and reservoir operation. To that avail, statistical models based on autoregressive techniques, i.e., AR-, ARIMA- and ARIMAex-, which includes additional external regressors, and multiple linear regression- (MLR) models, are developed and applied in the study region. Teleconnections between ocean states and the local climate are investigated and used as extra external predictors in the ARIMAex- and the MLR-model and shown to enhance the accuracy of the short-term predictions significantly. However, as the ocean state – local climate teleconnective relationships provide only a one- to four-month ahead lead time, the ocean state indices can support only a one-season-ahead forecast. Hence, GCM- climate predictors are also suggested as an additional predictor-set for a more reliable and somewhat longer short-term forecast. For the preparation of “pre-warning” information for up-coming possible future climate change with potential adverse hydrological impacts in the study region, the long-term climate prediction methodology is applied. The latter is based on the downscaling of climate predictions from several single- and multi-domain GCMs, using the two well-known downscaling methods SDSM and LARS-WG and a newly developed MLR-downscaling technique that allows the incorporation of a multitude of monthly or daily climate predictors from one- or several (multi-domain) parent GCMs. The numerous downscaling experiments indicate that the MLR- method is more accurate than SDSM and LARS-WG in predicting the recent past 20th-century (1971-2000) long-term monthly climate in the region. The MLR-model is, consequently, then employed to downscale 21st-century GCM- climate predictions under SRES-scenarios A1B, A2 and B1. However, since the hydrological watershed model requires daily-scale climate input data, a new stochastic daily climate generator is developed to rescale monthly observed or predicted climate series to daily series, while adhering to the statistical and geospatial distributional attributes of observed (past) daily climate series in the calibration phase. Employing this daily climate generator, 30 realizations of future daily climate series from downscaled monthly GCM-climate predictor sets are produced and used as input in the SWAT- distributed watershed model, to simulate future streamflow and other hydrological water budget components in the study region in a multi-realization manner. In addition to a general examination of the future changes of the hydrological regime in the KY-basin, potential future changes of the water budgets of three main reservoirs in the basin are analysed, as these are a major source of water supply in the study region. The results of the long-term 21st-century downscaled climate predictions provide evidence that, compared with the past 20th-reference period, the future climate in the study area will be more extreme, particularly, for SRES A1B. Thus, the temperatures will be higher and exhibit larger fluctuations. Although the future intensity of the rainfall is nearly constant, its spatial distribution across the region is partially changing. There is further evidence that the sequential rainfall occurrence will be decreased, so that short periods of high intensities will be followed by longer dry spells. This change in the sequential rainfall pattern will also lead to seasonal reductions of the streamflow and seasonal changes (decreases) of the water storage in the reservoirs. In any case, these predicted future climate changes with their hydrological impacts should encourage water planner and policy makers to develop adaptation strategies to properly handle the future water supply in this area, following the guidelines suggested in this study.

Os efeitos da cultura nas relações entre estilo de liderança, confiança e comprometimento: comparando equipes de operações especiais no Brasil e Estados Unidos

Esse trabalho tem como objetivo compreender a influência da cultura no estilo de liderança em equipes de operações especiais, usando como referência teórica principal as pesquisas de Geert Hofstede sobre dimensões culturais. Buscamos entender como os elementos da cultura nacional e da cultura organizacional influenciam o estilo de liderança comparando equipes de operações especiais do Brasil e dos Estados Unidos. As unidades brasileiras estudadas foram o Batalhão de Operações Especiais (BOPE) da Polícia Militar do Rio de Janeiro e a Coordenadoria de Recursos Especiais (CORE) da Polícia Civil do Rio de Janeiro. A equipe de operações especiais estudada nos Estados Unidos foi a SWAT. Os resultados apontam para a influência da cultura organizacional, e não da cultura nacional, no estilo de liderança.

Simulação da produção de sedimentos na bacia hidrográfica do Rio Pardo – Botucatu, SP, por modelagem hidrológica

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Morfometria de compartimentos hidrológicos e qualidade hídrica do município de Batatais-SP

Pós-graduação em Agronomia (Produção Vegetal) - FCAV

Análise espacial do conteúdo de água da bacia hidrográfica do Rio Pardo

O presente trabalho tem por objetivo avaliar a distribuição espacial, por geoestatística, da produção de água gerada pelo modelo hidrológico matemático SWAT 2009 (Soil and Water Assessment Tool, versão 2009), da parte inicial da bacia hidrográfica do Rio Pardo – SP. Foi utilizado um Sistema de Informação Geográfica (SIG) associado a uma interface com o modelo SWAT para a confecção do banco de dados. Para isto, as informações de entrada necessárias para avaliar a produção de lâmina de água (mm), que infiltrou e armazenou em cada sub-bacia gerada pelo SWAT, referem-se a dados tabulares climáticos e de parâmetros físicos e químicos de solo e a planos de informações como: o Modelo Numérico do Terreno (MNT), Mapa de Uso do Solo e Mapa de Solos. A amostragem geoestatística foi representada por uma malha irregular georreferenciada com 43 pontos localizados na parte central de cada sub-bacia representando a quantidade de água produzida. A análise geoestatística foi realizada pela construção dos variogramas e posteriormente a confecção dos mapas interpolados por krigagem. Do resultado obtido observou-se que a produção de água apresentou dependência espacial e que esta ocorreu de forma homogênea, tanto para os maiores como para os menores valores de produção de água encontrados na bacia.

Geotecnologias aplicadas à análise do assoreamento de reservatórios de hidrelétricas em cenário de escassez de dados de séries históricas

Pós-graduação em Engenharia Mecânica - FEG

Modelagem do aporte de sedimentos aplicada à bacia hidrográfica contribuinte da PCH Costa Rica (MS) e proposta de mitigação do assoreamento

Pós-graduação em Engenharia Mecânica - FEG

Espacialização dos sedimentos produzidos na parte inicial da bacia hidrográfica do Rio Pardo, Botucatu/SP

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Sediment yield reduction in an agricultural watershed

With proper application of Best Management Practices (BMPs), the impact from the sediment to the water bodies could be minimized. However, finding the optimal allocation of BMP can be difficult, since there are numerous possible options. Also, economics plays an important role in BMP affordability and, therefore, the number of BMPs able to be placed in a given budget year. In this study, two methodologies are presented to determine the optimal cost-effective BMP allocation, by coupling a watershed-level model, Soil and Water Assessment Tool (SWAT), with two different methods, targeting and a multi-objective genetic algorithm (Non-dominated Sorting Genetic Algorithm II, NSGA-II). For demonstration, these two methodologies were applied to an agriculture-dominant watershed located in Lower Michigan to find the optimal allocation of filter strips and grassed waterways. For targeting, three different criteria were investigated for sediment yield minimization, during the process of which it was found that the grassed waterways near the watershed outlet reduced the watershed outlet sediment yield the most under this study condition, and cost minimization was also included as a second objective during the cost-effective BMP allocation selection. NSGA-II was used to find the optimal BMP allocation for both sediment yield reduction and cost minimization. By comparing the results and computational time of both methodologies, targeting was determined to be a better method for finding optimal cost-effective BMP allocation under this study condition, since it provided more than 13 times the amount of solutions with better fitness for the objective functions while using less than one eighth of the SWAT computational time than the NSGA-II with 150 generations did.