Дисертації з теми "Indonesia Climate"
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Trimarianto, Ciptadi. "Thermal efficient dwelling design, Bali, Indonesia." Thesis, University of Newcastle Upon Tyne, 2003. http://hdl.handle.net/10443/474.
Повний текст джерелаPermana, Donaldi Sukma. "Reconstruction of Tropical Pacific Climate Variability from Papua Ice Cores, Indonesia." The Ohio State University, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=osu1449155469.
Повний текст джерелаChandrasa, Ganesha Tri. "Evaluation of Regional Climate Model Simulated Rainfall over Indonesia and its Application for Downscaling Future Climate Projections." The Ohio State University, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=osu1523464961178694.
Повний текст джерелаMulyasari, Farah. "Enhancing Climate-related Disaster Resilience through Effective Risk Communication in Bandung, Indonesia." Master's thesis, 京都大学 (Kyoto University), 2014. http://hdl.handle.net/2433/188880.
Повний текст джерелаPermana, Donaldi Sukma. "Climate, Precipitation Isotopic Composition and Tropical Ice Core Analysis of Papua, Indonesia." The Ohio State University, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=osu1313480990.
Повний текст джерелаMoody, Louise Dawn. "Indonesian climate investigations using stable isotopic data from modern, Holocene and Pliocene corals." Thesis, University of Canterbury. Geological Sciences, 2012. http://hdl.handle.net/10092/6729.
Повний текст джерелаMiyaguchi, Takaaki. "Climate Change Impact Reduction through Corporate Community Interface -Cases from India and Indonesia-." 京都大学 (Kyoto University), 2008. http://hdl.handle.net/2433/123773.
Повний текст джерелаKincaid, Joni L. "An assessment of regional climate trends and changes to the Mt. Jaya glaciers of Irian Jaya." Texas A&M University, 2003. http://hdl.handle.net/1969.1/5804.
Повний текст джерелаMulyani, Mari. "The interplay between the REDD+ mechanism and forest-related institutions in Indonesia." Thesis, University of Oxford, 2014. http://ora.ox.ac.uk/objects/uuid:23a98db8-6cc6-4e32-a82c-1e4eb069338a.
Повний текст джерелаAliloedin, Wiwin Widiyanti [Verfasser]. "Climate challenge and water scarcity adaptation strategies in the area of Pacitan, Indonesia / Wiwin Widiyanti Aliloedin." Gießen : Universitätsbibliothek, 2014. http://d-nb.info/106887421X/34.
Повний текст джерелаPutri, Siska Purnamasari. "Burden Sharing of Climate Change : Should Indonesia Be Held Responsible for Its Deforestation and Transboundary Haze?" Thesis, Linköpings universitet, Institutionen för kultur och samhälle, 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-166824.
Повний текст джерелаSzulecka, Julia. "Changing Paradigms in a Changing Climate." Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2015. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-188777.
Повний текст джерелаLukito, Jose Arif. "Framework for climate change adaptation for incorporation in public asset management: An Indonesian context." Thesis, Queensland University of Technology, 2018. https://eprints.qut.edu.au/119687/9/Jose%20Arif%20Lukito%20Thesis.pdf.
Повний текст джерелаKorkeala, Outi Kaarina. "Climate and land in turmoil : welfare impacts of extreme weather events and palm oil production expansion in Indonesia." Thesis, University of Sussex, 2011. http://sro.sussex.ac.uk/id/eprint/40054/.
Повний текст джерелаThibault, Mary Grace. "Modeling seagoing migration of early Homo via paleoclimate drift experiments to Sulawesi, Indonesia." The Ohio State University, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=osu1555500422012595.
Повний текст джерелаWestaway, Kira E. "Reconstructing the Quaternary landscape evolution and climate history of western Flores an environmental and chronological context for an archaeological site /." Access electronically, 2006. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20070117.170105/index.html.
Повний текст джерелаHowley, Brian, and Marc Fleischer. "Solar PV Powered Air Conditioner Analysis for an Office/Classroom in a Tropical Climate." Thesis, Högskolan Dalarna, Energiteknik, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:du-19038.
Повний текст джерелаArias, Ruiz Camilo. "High resolution climate records from modern and last interglacial periods derived from giant clam shells (Tridacnidae) in Sulawesi, Indonesia." Thesis, Nantes, 2017. http://www.theses.fr/2017NANT4081/document.
Повний текст джерелаGiant clam shells (Tridacnidae family) were used to reconstruct climatic conditions during the last interglacial periods in Indonesia's Sulawesi Island. Geochemical analyzes on modern shells have shown that these organisms actually record the variation of the environment in which they live, in terms of: temperature, salinity, precipitation and nutrient inputs. The main results were the reproducibility of the geochemical signal in two different species, as well as the recording of the climatic anomalies related to the La Niña phenomenon in 2010. Uranium-series dating revealed reefs formed at the beginning of the last interglacial period (MIS-5) and the penultimate interglacial or MIS-7. The comparison between modern and fossil reconstructions gave the following main results: 1) colder average temperature conditions with reduced seasonality for both periods (beginning of MIS-5 and MIS-7) due to drier conditions.2) These parameters respond systematically to a decrease / increase of the sea level and testify the strong interaction between the atmospheric and ocean circulation in the region3) The interannual variability of SST / SSS presents oscillations in the same amplitude as today for the MIS-5 period, however for MIS 7, these oscillations are reduced around 50% compared to the current interglacial4) The Mg/Ca ratio has a strong taxonomic variation, additional studies are needed to remove the biological factor related to geochemical signal. 5) Ba/Ca present a potential use as tracers of upwelling processes and/ or variations in salinity. Giant clam shells (Tridacnidae family) were used to reconstruct climatic conditions during the last interglacial periods in Indonesia's Sulawesi Island. Geochemical analyzes on modern shells have shown that these organisms actually record the variation of the environment in which they live, in terms of: temperature, salinity, precipitation and nutrient inputs. The main results were the reproducibility of the geochemical signal
Wurtzel, Jennifer Beth. "Reading the Rain in Rocks: A late deglacial speleothem record from Sumatra, Indonesia." Phd thesis, Canberra, ACT : The Australian National University, 2017. http://hdl.handle.net/1885/143191.
Повний текст джерелаHansson, Robin, and Elena Mokeeva. "Securing resilience to climate change impacts in coastal communities through an environmental justice perspective: A case study of Mangunharjo, Semarang, Indonesia." Thesis, KTH, Miljöstrategisk analys (fms), 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-175468.
Повний текст джерелаSiswanto, Shantosa Yudha. "Impact Evaluation of Future Climate and Land Use Scenarios on Water and Sediment Regime using Distributed Hydrological Modelling in a Tropical Rainforest Catchment in West Java (Indonesia)." Doctoral thesis, Universitat Politècnica de València, 2020. http://hdl.handle.net/10251/153152.
Повний текст джерела[ES] El cambio climático ha afectado a Indonesia, por ejemplo, incrementando la temperatura del aire en la superficie, incluso en la cuenca del Upper Citarum. Este fenómeno conduce a la falta de agua en la estación seca, reduciendo la producción agrícola lo que es un gran obstáculo para su actividad. Además, la actividad humana ha producido cambios severos en LULC en la cuenca del Upper Citarum, Indonesia. Esto se debe al elevado crecimiento de la población en la región, por el que se han convertido campos de arroz y áreas boscosas en suelo urbano. De esta forma, el objetivo general de esta tesis es comprender y analizar el impacto de los cambios climáticos y LULC en el proceso hidrológico y su relación con los cambios históricos y futuros mediante el uso de modelos distribuidos espacialmente en la cuenca tropical del Upper Citarum. El modelo distribuido TETIS se ha implementado para obtener los resultados de escenarios pasados y futuros en los ciclos de agua y sedimentos. Se usaron batimetrías históricas anuales en el embalse para calibrar y validar el submodelo de sedimentos que involucra la evolución de la densidad de Miller y la eficiencia de retención de la ecuación de Brune. Con el fin de arrojar más luz sobre estos problemas, el escenario de cambio climático se ha implementado en base al modelo de cambio climático bajo las trayectorias RCP 45 y RCP 85. Además, para intentar resolver el problema LULC, también se ha implementado el LULC histórico y futuro. El modelo LCM se usó para pronosticar el LULC en 2029 y los resultados muestran, por un lado, una continuación en la expansión de las áreas urbanas a expensas de los arrozales contiguos. Los resultados determinaron que la deforestación y la urbanización fueron los factores más influyentes para la alteración de los procesos hidrológicos y sedimentológicos en la cuenca del Upper Citarum. Por lo tanto, disminuye la evapotranspiración, aumenta la producción de agua al aumentar todos sus componentes; escorrentía, interflujo y flujo base. Los cambios en LULC están produciendo y producirán, un incremento relativamente pequeño de las tasas de erosión, aumentando el área excede la erosión de Tsl. La producción de sedimentos aumentará en 2029 como resultado del incremento de la erosión. Se espera que otros escenarios de LULC como la conservación, el plan gubernamental y los escenarios de vegetación natural tengan un incremento en la evapotranspiración total, y se espera que la producción de agua disminuya. El régimen de inundación, la erosión y la sedimentación se reducen drásticamente. Por lo tanto, habrá un incremento de la vida útil del embalse y la energía hidroeléctrica. El cambio climático altera la magnitud del equilibrio hídrico y puede identificarse a partir del cambio de infiltración, escorrentía, interflujo, flujo base y producción de agua. Esos incrementos finalmente cambian el régimen de inundación y erosión de la cuenca. La trayectoria RCP 85 tiene un mayor impacto en comparación con la trayectoria RCP 45 en el ciclo hidrológico y de sedimentos. El cambio de LULC tiene un mayor impacto en el balance hídrico, el régimen de inundación, la erosión y la sedimentación. La combinación del cambio climático y LULC tiene un mayor impacto en los flujos de equilibrio hídrico, erosión, inundación, sedimentación y será catastrófico para la operación hidroeléctrica de la presa Saguling.
[CA] El canvi climàtic ha afectat Indonèsia, per exemple, incrementant la temperatura de l'aire en la superfície, inclús en la conca de l'Upper Citarum. Aquest fenomen conduïx a la falta d'aigua en l'estació seca, reduint la producció agrícola, el que és un gran obstacle per a la seua activitat. A més, l'activitat humana ha produït canvis severs en LULC en la conca de l'Upper Citarum, Indonèsia. Açò es deu a l'elevat creixement de la població en la regió, motiu pel qual s'han anat convertint camps d'arròs i àrees boscoses en sòl urbà. D'aquesta manera, l'objectiu general d'aquesta tesi és comprendre i analitzar l'impacte dels canvis climàtics i LULC en el procés hidrològic i la seua relació amb els canvis històrics i futurs per mitjà de l'ús de models distribuïts espacialment en la conca tropical de l'Upper Citarum. El model distribuït TETIS s'ha implementat per a obtindre els resultats d'escenaris passats i futurs en els cicles de l'aigua i sediments. Es van usar batimetries històriques anuals en l'embassament per a calibrar i validar el submodel de sediments que involucra l'evolució de la densitat de Miller i l'eficiència de retenció de l'equació de Brune. Amb la finalitat de donar més llum a aquests problemes, l'escenari de canvi climàtic s'ha implementat basant-se en el model de canvi climàtic davall les trajectòries RCP 45 i RCP 85. A més, per a intentar resoldre el problema LULC, també s'ha implementat el LULC històric i futur. El model LCM es va usar per a pronosticar el LULC en 2029 i els resultats mostren, d'una banda, una continuació en l'expansió de les àrees urbanes a costa dels arrossars contigus. Els resultats van determinar que la desforestació i la urbanització van ser els factors més influents per a l'alteració dels processos hidrològics i sedimentològics en la conca de l'Upper Citarum. Per tant, disminuïx l'evapotranspiració, augmenta la producció d'aigua en augmentar tots els seus components; escorrentia, interflux i flux base. Els canvis en LULC estan produint i produiran, un increment relativament xicotet de les taxes d'erosió, augmentant l'àrea excedix l'erosió de Tsl. La producció de sediments augmentarà en 2029 com a resultat de l'increment de l'erosió. S'espera que altres escenaris de LULC com la conservació, el pla governamental i els escenaris de vegetació natural tinguen un increment en l'evapotranspiració total, i s'espera que la producció d'aigua disminuïsca. El règim d'inundació, l'erosió i la sedimentació es reduïxen dràsticament. Per tant, hi haurà un increment de la vida útil de l'embassament i l'energia hidroelèctrica. El canvi climàtic altera la magnitud de l'equilibri hídric i pot identificar-se a partir del canvi d'infiltració, escorrentia, interflux, flux base i producció d'aigua. Eixos increments finalment canvien el règim d'inundació i erosió de la conca. La trajectòria RCP 85 té un major impacte en comparació amb la trajectòria RCP 45 en el cicle hidrològic i de sediments. El canvi de LULC té un major impacte en el balanç hídric, el règim d'inundació, l'erosió i la sedimentació. La combinació del canvi climàtic i LULC té un major impacte en els fluxos d'equilibri hídric, erosió, inundació, sedimentació i serà catastròfic per a l'operació hidroelèctrica de la presa Saguling.
thank the Directorate General of Higher Education of Indonesia (DIKTI), for granting me the opportunity to pursue PhD study and adventure in Europe. The authors are also thankful to the Spanish Ministry of Economy and Competitiveness through the research projects TETISMED (CGL2014-58127-C3-3-R) and TETISCHANGE (RTI2018-093717-B-I00).
Siswanto, SY. (2020). Impact Evaluation of Future Climate and Land Use Scenarios on Water and Sediment Regime using Distributed Hydrological Modelling in a Tropical Rainforest Catchment in West Java (Indonesia) [Tesis doctoral no publicada]. Universitat Politècnica de València. https://doi.org/10.4995/Thesis/10251/153152
TESIS
Lindblom, Petersson Malin. "REDD+ : A case study of the challenges weak land rights in Indonesia pose for equitable distribution of benefits from activities to mitigate climate change." Thesis, Uppsala universitet, Statsvetenskapliga institutionen, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-274185.
Повний текст джерелаYamamoto, Kodai. "ASSESSMENT OF CLIMATE AND LAND USE CHANGE IMPACTS ON FLOOD INUNDATION IN A HUMID TROPICAL RIVER BASIN:A CASE STUDY OF SUMATRA ISLAND IN INDONESIA." Doctoral thesis, Kyoto University, 2021. http://hdl.handle.net/2433/263624.
Повний текст джерела京都大学
新制・課程博士
博士(工学)
甲第23163号
工博第4807号
京都大学大学院工学研究科社会基盤工学専攻
(主査)教授 立川 康人, 教授 田中 茂信, 准教授 佐山 敬洋
学位規則第4条第1項該当
Doctor of Philosophy (Engineering)
Kyoto University
DFAM
Mujizat, Danar Anindito. "The Sovereign Green Sukuk: An Analysis of Its Process and Barriers to Funding Renewable Energy Projects in Indonesia." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-445408.
Повний текст джерелаBaram, Laura, and Sara Yaghi. ""No matter how safe we play, we are all subjects to Mother Nature's whims." : A qualitative study of how Swedish companies perceive the risks from climate change and natural disasters in Indonesia." Thesis, Linnéuniversitetet, Institutionen för marknadsföring (MF), 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-53520.
Повний текст джерелаPardon, Lénaïc. "Modelling of the nitrogen budget of oil palm plantations to help reduce losses to the environment. Case study in Sumatra, Indonesia." Thesis, Paris, Institut agronomique, vétérinaire et forestier de France, 2017. http://www.theses.fr/2017IAVF0018/document.
Повний текст джерелаHumanity faces the challenges of urgently decreasing the environmental impact of agriculture, shifting diets and increasing food production. Oil palm is a tropical perennial crop emblematic of these challenges. While its cultivation can be associated with environmental impacts, oil palm can produce 3 to 7 t of edible oil ha-1 in optimal conditions, which is 7 to 10 fold higher than in annual oil crops. In this context, improving palm oil production sustainability is crucial for both reducing negative environmental impacts and ensuring food security. Application of synthetic nitrogen (N) fertilisers was identified as a major source of environmental impacts associated with the cultivation of oil palm. Life cycle assessments of palm oil have already been performed to help quantify impacts and identify potential improvements of management practices. However, the only available emission models to estimate N losses to environment are generally valid for annual crops and temperate climate conditions. The use of such general models in life cycle assessment may lead to very uncertain results or to low sensitivity of assessments to management practices. The overall objective of this research work was to help identify management practices to reduce N losses in the environment. The core of the work was hence to develop a model that estimates all N losses in oil palm plantations, while being sensitive to management practices. The study focused on N fluxes in industrial oil palm plantations on mineral soils. We performed four steps in order to complete the objectives of this research work. First, we conducted a literature review of all the existing knowledge about N fluxes and losses in plantations. Second, we compared 11 existing models that may be used to predict N losses in plantations. Third, we performed an in-depth Morris’s sensitivity analysis of one of the models, the APSIM-Oil palm process-based model. Fourth, we used all the information identified in the previous chapters, together with expert knowledge, to build IN-Palm, an agri-environmental indicator for N losses in oil palm plantations. We used the INDIGO® method and the fuzzy decision tree modelling approach to develop IN-Palm, and we validated this indicator using a field dataset of N leaching from a plantation in Sumatra, Indonesia. Our literature review and model comparison showed that oil palm peculiarities may impact significantly N dynamics and losses. We identified research gaps and uncertainties about N losses, their drivers and the modelling of oil palm peculiarities. We identified the main drivers of N losses and yield in the APSIM-Oil palm processbased model. We built IN-Palm, which uses 21 readily available input variables to estimate each N loss pathway. IN-Palm predictions of N leaching were acceptable, and IN-Palm has shown efficient to help testing management changes. This research constitutes a comprehensive synthesis of the available knowledge and models for N fluxes and losses in oil palm plantations. One of the main results is a novel agri-environmental indicator, IN-Palm, operationally-oriented, sensitive to local practices and environmental conditions, as well as potentially useable as an emission model for holistic approaches such as life cycle assessment. The INDIGO® method and fuzzy decision tree modelling approach were shown to be very well adapted for building agri-environmental indicators in contexts of knowledge scarcity. This indicator can be a useful base for further research about using agrienvironmental indicators to reduce uncertainty in life cycle assessment, and for future adaptations for other tropical perennial crops
Pettersson, Tobar Rebecka. "A more sustainable Palm oil industry : A case study on the Government in Indonesia achieving SDGs number 8 and 13 with the help of the palm oil industry." Thesis, Linnéuniversitetet, Institutionen för samhällsstudier (SS), 2020. http://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-98037.
Повний текст джерелаPardon, Lénaïc. "Modelling of the nitrogen budget of oil palm plantations to help reduce losses to the environment. Case study in Sumatra, Indonesia." Thesis, Paris, Institut agronomique, vétérinaire et forestier de France, 2017. https://researchonline.jcu.edu.au/52952/1/52952-pardon-2017-thesis.pdf.
Повний текст джерелаAldrian, Edvin. "Simulation of Indonesian rainfall with a hierarchy of climate models." Hamburg : Max-Planck-Inst. für Meteorologie, 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=968789773.
Повний текст джерелаBiagioni, Siria [Verfasser], Hermann [Akademischer Betreuer] [Gutachter] Behling, Erwin [Gutachter] Bergmeier, and Dietrich [Gutachter] Hertel. "Long-term dynamics of tropical rainforests, climate, fire, human impact and land-use change in Indonesia : A focus on the montane rainforests in Central Sulawesi and peat-swamp rainforests in Sumatra / Siria Biagioni. Betreuer: Hermann Behling. Gutachter: Hermann Behling ; Erwin Bergmeier ; Dietrich Hertel." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2016. http://d-nb.info/1102535702/34.
Повний текст джерелаSuwarno, Yogi. "Responding to climate change : policy integration and the Indonesian forestry sector." Thesis, University of Birmingham, 2017. http://etheses.bham.ac.uk//id/eprint/7694/.
Повний текст джерелаHughes, Tertia. "Indonesian throughflow and its effect on the climate of the Indian Ocean." Thesis, McGill University, 1991. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=60072.
Повний текст джерелаThe stronger Sverdrup circulation dominates the thermohaline circulation in most of the model ocean except near the eastern boundary.
The western boundary currents apparently play a very minor role in this basinwide thermohaline circulation. This differs from the warm water route proposed by Gordon (1986), and supports the alternative hypothesis that the heat from the equatorial Pacific is returned to the South Atlantic via the eastward-flowing Antarctic Circumpolar Current rather than past the Agulhas Retroflection.
The Indonesian throughflow is shown to significantly affect the surface heat fluxes and the meridional heat transport in the Indian Ocean. The role of the throughflow in maintaining the very warm climate of the Indian Ocean (a net exporter of heat) is described.
Large-scale, fairly long period ($>$100 days) barotropic eddies are found in the western portion of the basin for some solutions.
Jaenicke, Julia. "3D modelling and monitoring of Indonesian peatlands aiming at global climate change mitigation." Diss., lmu, 2010. http://nbn-resolving.de/urn:nbn:de:bvb:19-117610.
Повний текст джерелаSchollaen, Karina. "Tracking climate signals in tropical trees : new insights from Indonesian stable isotope records." Phd thesis, Universität Potsdam, 2014. http://opus.kobv.de/ubp/volltexte/2014/7194/.
Повний текст джерелаDie tropischen Gewässer um Indonesien sind eine der äquatorialen Wärme- und Feuchtigkeitsquellen, die als treibende Kraft des globalen Klimasystems betrachtet werden können. Das Klima in Indonesien ist geprägt durch das Australisch-Indonesische Monsunsystem. Weiterhin besteht eine Verknüpfung mit El Niño-Southern Oszillation (ENSO) Ereignissen, die oft zu schweren Dürren oder Überschwemmungen in der Region mit tiefgreifenden gesellschaftlichen und wirtschaftlichen Folgen führen. Der neueste IPCC-Bericht legt dar, dass ENSO auch in den nächsten 100 Jahren das vorherrschende Klimaphänomen im tropischen Pazifik bleiben wird. Ferner wird davon ausgegangen, dass sich die ENSO-bezogenen Niederschlagsextrema intensivieren werden. Wenig Übereinstimmung herrscht jedoch bislang zwischen den Klimasimulationsmodellen in Bezug auf die voraussichtlichen Veränderungen von ENSO und dem Australisch-Indonesischen Monsunsystem. Hochaufgelöste Paläoklima-Archive, wie z.B. Jahrringe oder warvierte Seesedimente, geben Auskunft über die natürliche Klimavariabilität der Vergangenheit und können somit dazu beitragen, die Computersimulationen der künftigen Klimaentwicklung zu verbessern und zu validieren. Hundertjährige stabile Jahrring-Isotopenchronologien | Das Hauptziel dieser Doktorarbeit war es, dass Potenzial von tropischen Jahrringen zur Aufzeichnung von Klimasignalen herauszustellen und deren Evaluierung als Paläoklimaproxys. Im Detail wurden stabile Kohlenstoff- (δ13C) und Sauerstoff- (δ18O) Isotopenverhältnisse in Teakbäumen analysiert, und die ersten gut replizierten hundertjährigen (AD 1900-2007) stabilen Isotopenchronologien aus Java (Indonesien) erstellt. Dabei wurden verschiedene klimatische Einflussgrößen getestet, ob diese signifikante Korrelationen mit den Jahrringparametern aufzeigen. Weiterhin wurden hochaufgelöste intra-annuelle Sauerstoffisotopenzeitreihen erstellt, um den Transfer des saisonalen Niederschlagssignals in den jeweiligen Jahrring zu bemessen. Die ermittelte Sauerstoff-Isotopenchronologie wurde anschließend auf mögliche ENSO Signale hin untersucht. Methodische Errungenschaften | Ein zweites Ziel dieser Arbeit war es neue Verfahren zur Analyse stabiler Isotope in Baumjahrringen zu entwickeln und zu optimieren. Zwei verschiedene UV-Lasermikrodissektions-Systeme wurden getestet als neues präzises Präparationswerkzeug für stabile Isotopenstudien. Darüber hinaus wurde eine verbesserte Methode für die Probenaufbereitung stabiler Isotopenmessungen anhand von Zellulose-Dünnschnitten entwickelt. Die wichtigsten Ergebnisse dieser Doktorarbeit sind: I) Die hier vorgestellten neuartigen Techniken zu Probenvorbereitung verbessern die Analyse stabiler Isotope für Jahrringstudien in Hinsicht auf Präzision, Effizienz und Qualität. Es wurde gezeigt, dass die UV-Lasermikrodissektion eine wertvolle Technik ist, um die Beprobung von Pflanzengewebe in höchster Auflösung und beispielloser Präzision durchzuführen. II) Es ist gelungen, einen Leitfaden für ein modifiziertes Verfahren der Zelluloseextraktion an Gesamtholz-Dünnschnitten und der anschließenden Jahrringaufbereitung zu erstellen. Diese neuartige Methode optimiert die Analyse stabiler Isotopenzeitreihen in zweierlei Hinsicht: schnellere und effiziente Zelluloseextraktion und präzise Trennung der Jahrringsequenzen in inter-annueller bis intra-annuelle Auflösung. III) Die hundertjährigen stabilen Jahrring-Isotopenchronologien weisen signifikante Korrelationen mit dem regionalen Niederschlag auf. In den hochaufgelösten stabilen Sauerstoffisotopenwerten spiegelt sich deutlich das Niederschlagssignal der Trocken- und der Regenzeit wieder. IV) Die stabile Sauerstoffisotopenzeitreihe zeigt signifikante Korrelationen mit verschiedenen ENSO Phasen. Dies betont, dass die verschiedenen ENSO Phasen bei der Interpretation von tropischen Paläodaten zu berücksichtigen sind. Die Ergebnisse der Dissertation zeigen, dass saisonal aufgelöste stabile Sauerstoffisotopenchronologien von indonesischen Teakbäumen ein geeigneter Proxy für mehrhundertjährige Rekonstruktionen der regionalen Niederschlagsvariabilität (Monsun-Signale) und großräumiger Ozean-Atmosphären-Systeme (ENSO) für den Indopazifik ist. Darüber hinaus bieten die neuartigen methodischen Errungenschaften viele neue Ansätze für multidisziplinäre hochaufgelöste Studien in der paläoklimatologischen Forschung.
Rahman, Arif Budi. "Mainstreaming Climate Change Adaptation in a Developing Country Context: an Indonesian Case Study." Thesis, Curtin University, 2017. http://hdl.handle.net/20.500.11937/59733.
Повний текст джерелаFrigola, Amanda [Verfasser], Matthias [Akademischer Betreuer] Prange, Michael [Gutachter] Schulz, and Georg [Gutachter] Feulner. "Global climate and Indonesian Throughflow during the Middle Miocene Climate Transition : a modeling approach / Amanda Frigola ; Gutachter: Michael Schulz, Georg Feulner ; Betreuer: Matthias Prange." Bremen : Staats- und Universitätsbibliothek Bremen, 2019. http://d-nb.info/1196286299/34.
Повний текст джерелаAdriansyah, Willy. "Combined Air Conditioning and Tap Water Heating Plant, Using CO2 as Refrigerant for Indonesian Climate Condition." Doctoral thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for energi- og prosessteknikk, 2001. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-2023.
Повний текст джерелаDamanik, Enceria. "Principal leadership style and its impact on school climate and teacher self-efficacy in Indonesian schools." Thesis, Curtin University, 2014. http://hdl.handle.net/20.500.11937/391.
Повний текст джерелаKaras, Cyrus [Verfasser]. "Mid-Pliocene restriction of the Indonesian Gateway and its implication on ocean circulation and climate / Cyrus Karas." Kiel : Universitätsbibliothek Kiel, 2010. http://d-nb.info/1019985100/34.
Повний текст джерелаSchollaen, Karina [Verfasser], and Achim [Akademischer Betreuer] Brauer. "Tracking climate signals in tropical trees : new insights from Indonesian stable isotope records / Karina Schollaen. Betreuer: Achim Brauer." Potsdam : Universitätsbibliothek der Universität Potsdam, 2014. http://d-nb.info/1060257475/34.
Повний текст джерелаAdriansyah, Willy. "Combined Air Conditioning and Tap Water Heating Plant, Using CO2 as Refrigerant for Indonesian Climate Condition." Doctoral thesis, Norwegian University of Science and Technology, Department of Energy and Process Engineering, 2001. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-2023.
Повний текст джерелаA combined air-conditioning and water heating system using carbon dioxide as refrigerant has been investigated theoretically and experimentally. A computer program simulates the combined system has been developed and verified with experimental data. Effects of the following parameters to the system performance were examined: ratio of hot water load to rejected heat from air-conditioning system (load ratio), evaporation temperature, cooling medium temperature, inlet water temperature, hot water temperature, discharge pressure, and presence of internal heat exchanger. Main results were coefficient of performance and cooling capacity.
It was concluded that there is an optimum pressure where the system reaches the highest coefficient of performance. Variation of coefficient of performance of the combined system with discharge pressures is similar to that of the airconditioning system without heat recovery.
Load ratio affects the performance of the air-conditioning side. Coefficient of performance of the air-conditioning side (cooling-COP) increased with increasing load ratio. Optimum discharge pressure was affected by load ratio.
Improvement of cooling-COP depends on both cooling medium and inlet water temperatures. The cooling-COP was lower at higher cooling medium temperature and higher inlet water temperature. When inlet water temperature is higher than cooling medium temperature, the cooling-COP will be lower compared to the airconditioning system without heat recovery.
The system performance decreased as hot water temperature increased. The decrease is due to a need for higher discharge temperature to achieve maximum cooling-COP.
Internal heat exchanger plays an important role in achieving higher system performance. Coefficient of performance is higher for the combined system with internal heat exchanger. The length of internal heat exchanger affects the cooling-COP and the location of the optimum discharge pressure.
Estimation results used for calculating annual energy consumption in various type of buildings show that the largest energy saving can be achieve in hospitals, followed by in hotels and in multifamily buildings. Simple comparison of combined CO2 system with separated R22 and stand-alone water heating system show better total system efficiency for CO2 system.
Aswi. "Bayesian spatio-temporal modelling of small areas: Dengue fever in Makassar Indonesia." Thesis, Queensland University of Technology, 2020. https://eprints.qut.edu.au/200547/1/_Aswi_Thesis.pdf.
Повний текст джерелаBolliet, Timothé [Verfasser]. "West Pacific climate and circulation over the last 160 kyr : a palaeontological and geochemical multiproxy reconstruction within the inflow path of the Indonesian Throughflow / Timothé Geoffroy Bolliet." Kiel : Universitätsbibliothek Kiel, 2011. http://d-nb.info/102020205X/34.
Повний текст джерелаAldrian, Edvin [Verfasser]. "Simulation of Indonesian rainfall with a hierarchy of climate models = Simulationen des Indonesischen Niederschlags mit einer Hierarchie von Klimamodellen / Max-Planck-Institut für Meteorologie. Von Edvin Aldrian." Hamburg : Max-Planck-Inst. für Meteorologie, 2003. http://d-nb.info/968789773/34.
Повний текст джерелаLe, Blanc Jean-Luc. "The role of the Indian Ocean in the global climate system : the propagation of Indian Ocean Kelvin waves in the Indonesian Seas and their influence on western Pacific sea level variability." Thesis, University of Southampton, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.402544.
Повний текст джерелаHapsari, Kartika Anggi [Verfasser], Hermann [Akademischer Betreuer] Behling, Alexander [Gutachter] Schmidt, Thomas [Gutachter] Giesecke, Markus [Gutachter] Hauck, and Tim Dr [Gutachter] Jennerjahn. "Indonesian coastal wetlands : The past dynamics of environment and carbon, the potential for climate change mitigation and the assessment for conservation, management and restoration / Kartika Anggi Hapsari ; Gutachter: Alexander Schmidt, Thomas Giesecke, Markus Hauck, Tim Dr. Jennerjahn ; Betreuer: Hermann Behling." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2019. http://d-nb.info/1180720040/34.
Повний текст джерелаSabajo, Clifton. "Changements dans l’utilisation des terres et de la couverture terrestre en Asie du sud-est : les effets de la transformation sur les paramètres de la surface en Indonésie." Thesis, Paris, AgroParisTech, 2018. http://www.theses.fr/2018AGPT0005.
Повний текст джерелаOver the last decades, Indonesia has experienced dramatic land transformations with an expansion of oil palm plantations at the expense of tropical forests. Indonesia is currently one of the regions with the highest transformation rate of the land surface worldwide related to the expansion of oil palm plantations and other cash crops replacing forests on large scales. As vegetation is a modifier of the climate near the ground these large-scale land transformations have major impacts on surface biophysical variables such as land surface temperature (LST), albedo, vegetation indices (e.g. the normalized difference vegetation index, NDVI), on the surface energy balance and energy partitioning.Despite the large historic land transformation in Indonesia toward oil palm and other cash crops and governmental plans for future expansion, this is the first study so far to quantify the impacts of land transformation on biophysical variables in Indonesia. To assess such changes at regional scale remote sensing data are needed.As a key driver for many ecological functions, LST is directly affected by land cover changes.We analyze LST from the thermal band of a Landsat image and produce a high-resolution surface temperature map (30 m) for the lowlands of the Jambi province in Sumatra (Indonesia), a region which experienced large land transformation towards oil palm and other cash crops over the past decades. The comparison of LST, albedo, NDVI, and evapotranspiration (ET) between seven different land cover types (forest, urban areas, clear cut land, young and mature oil palm plantations, acacia and rubber plantations) shows that forests have lower surface temperatures than the other land cover types, indicating a local warming effect after forest conversion. LST differences were up to 10.1 ± 2.6 ºC (mean ± SD) between forest and clear-cut land. The differences in surface temperatures are explained by an evaporative cooling effect, which offsets an albedo warming effect.Young and mature oil palm plantations differenced in their biophysical. To study the development of surface biophysical variables during the 20 – 25 years rotation cycle of oil palm plantations, we used three Landsat images from the Jambi province in Sumatra/Indonesia covering a chronosequence of oil palm plantations.Our results show that differences between oil palm plantations in different stages of the oil palm rotation cycle are reflected in differences in the surface energy balance, energy partitioning and biophysical variables. During the oil palm plantation lifecycle the surface temperature differences to forest gradually decrease and approach zero around the mature oil palm plantation stage of 10 years. Concurrently, NDVI increases and the albedo decreases approaching typical values of forests. The surface energy balance and energy partitioning show a development patterns related to biophysical variables and the age of the oil palm plantations. Newly established and young plantations (< 5 years) have less net radiation available than mature oil palm plantations, yet have higher surface temperatures than mature oil palm plantations. The changes in biophysical variables, energy balance and energy partitioning during the oil palm rotation cycle can be explained by the previously identified evaporative cooling effect in which the albedo warming effect is offset. A main determinant in this mechanism is the vegetation cover during the different phases in the oil palm rotation cycle. NDVI as a proxy for vegetation cover showed a consistent inverse relation with the LST of different aged oil palm plantations, a trend that is also observed for different land use types in this study. (Last and final summary in the thesis)
Boun, Heng Mathias. "La sédimentation dans les lacs de barrage à Java, Indonésie : processus, rythmes et impacts." Thesis, Paris 1, 2013. http://www.theses.fr/2013PA010564/document.
Повний текст джерелаSince the Sixties, a large number of dams have been built in the Indonesian archipelago's main island, Java. Their rôle are multiple, going from liquid flows control (flood – peak shaving and low flow support) to water supply of great urban areas and agricultural lands. They also are an important energy supplier. After their watering, a fast filling of the tanks related to rates of erosion that appear among the highest in the world, has been observed. This significant efficiency decrease involves multiple negative impacts on environment and utilities. Through a multiple approach (GIS, remote sensing, hydroclimatic databases, lake surveys...), the objectives of this research are to determine the sedimentary transfer rates and pace within the studied basins, which act as erosion indicators in their respective basins. The key determinants affecting this high sedimentation will be highlighted and a software will be developed with the aim to provide Javanese river basins authorities with new tools
Gunawan, Lalu Adi. "Adapting to climate change: perspectives from rural communities in Lombok, eastern Indonesia." Thesis, 2015. https://researchonline.jcu.edu.au/46424/1/46424-gunawan-2015-thesis.pdf.
Повний текст джерелаGriffiths, Michael Lindgren. "Late-Pleistocene climate evolution of the southern sub-equatorial tropics from east-Indonesian speleothems." Thesis, 2010. http://hdl.handle.net/1959.13/807577.
Повний текст джерелаThe climate evolution of the southern sub-equatorial tropics during marine isotope stage (MIS)5a/b and the Holocene is explored using geochemical tracers from speleothems on Flores island, Indonesia. Oxygen isotope measurements from two precisely-dated stalagmites reveal that the Australian-Indonesian monsoon increased during the Younger Dryas (YD) cooling event, when Atlantic meridional overturning circulation was relatively weak. Monsoon precipitation intensified even more rapidly from 11 to 7 ka ago, when the Indonesian continental shelf was flooded by global sea-level rise. Analysis of oxygen (δ18O) and hydrogen (δD) isotope ratios from speleothem fluid inclusions shows that inclusion-δ18O values vary in phase with speleothem calcite δ18O during the Holocene, confirming that calcite δ18O primarily reflects variations in the δ18O of meteoric rainfall. Cave drip-water temperatures, reconstructed from coupled measurements of δ18O in speleothem calcite and fluid inclusions, remained relatively constant through the Holocene but were significantly cooler during the YD, consistent with the high northern latitudes. To help confirm the stable isotope records, trace elements were used to reconstruct the position of the austral summer inter-tropical convergence zone and east Indonesian rainfall variability during the Holocene. Mg/Ca and Sr/Ca ratios correlate significantly with one another, and with δ18O and δ13C, throughout the record suggesting that the trace element ratios were dominated by prior calcite precipitation, a process whereby degassing in the vadose zone during periods of low recharge causes deposition of calcite and disproportionate loss of Ca2+ ions (relative to Mg2+ and Sr2+) ‘upstream’ of the stalagmite. Comparison of speleothem δ18O time-series from Flores and Borneo shows that they vary in unison for much of the Holocene. However, there is an exception during the mid-Holocene when a distinct anomaly in δ18O in the Borneo record, possibly caused by a change in the circulation of the Australian-Indonesian summer monsoon (AISM) in response to a period of positive IOD-like conditions in the eastern Indian Ocean, occurred between the two regions. A stalagmite reconstruction of Indo-Pacific climate through the interval 84 - 91 ka shows that the lower-frequency oxygen isotope trend indicates that the AISM was largely controlled by local summer insolation during this time, while the carbon isotopes show a pattern that is closer linked with northern polar-latitude ice-core records. Most notably, an abrupt decrease in the temperature-controlled δ13C values at the MIS 5a/b transition occurs in parallel with GIS 21 in the GISP2 δ18O and CH4 records highlighting the strong connection between the IPWP and North Atlantic during the last glacial period.