Durante el fenómeno de “El Niño Costero 2017”, de consecuencias devastadoras para nuestro país, el gobierno del expresidente Pedro Pablo Kuczynski promovió encuadres informativos resaltando su gestión en la atención de la emergencia y trató de imponerlos en medios de comunicación como El Comercio y La República, entrando en una pugna por evitar que calen en el público los encuadres propios que al mismo tiempo generaron dichos diarios y otros actores. Conocer si el expresidente Kuczynski hizo prevalecer o no sus encuadres durante el tiempo que duró este fenómeno, en un contexto de inestabilidad avivado por el escándalo de corrupción del caso Lava Jato y una polarización exacerbada por la oposición política desde el Congreso de la República, es relevante debido a que permite establecer a través del framing cómo un presidente de la República busca construir una agenda, enmarcar la realidad mediática a su favor e implementar estrategias de comunicación exitosas en un escenario de permanente disputa. “El Niño Costero 2017” estuvo entre los sucesos noticiosos con mayor cobertura e impacto ese año. La elección de este acontecimiento responde al interés de analizar el desempeño del mandatario y su comunicación, que permitió un incremento de 11 puntos de la aprobación presidencial en un mes y llegó a 45% en marzo, de acuerdo a la encuestadora Datum; sin embargo, posteriormente no pudo mantener ese respaldo ciudadano. Los resultados de la presente investigación podrían convertirse en insumo importante para los responsables de las comunicaciones de la Presidencia de la República o de otras instancias de gobierno. / During the phenomenon of “El Niño Costero 2017”, with devastating consequences for our country, the government of former President Pedro Pablo Kuczynski promoted informative frames highlighting his management in addressing the emergency and tried to impose them in media outlets such as El Comercio and La República, entering into a struggle to prevent the public's own frames that at the same time generated by said newspapers and other actors. Knowing whether or not former President Kuczynski made his frames prevail during the time that this phenomenon lasted, in a context of instability fueled by the corruption scandal of the Lava Jato case and a polarization exacerbated by the political opposition from the Congress of the Republic, is relevant because it allows us to establish through framing how a president of the Republic seeks to build an agenda, frame the media reality in his favor and implement successful communication strategies in a scenario of permanent dispute. “El Niño Costero 2017” was among the news events with the greatest coverage and impact that year. The choice of this event responds to the interest of analyzing the president's performance and his communication, which allowed an increase of 11 points in presidential approval in one month and reached 45% in March, according to the pollster Datum; However, he was subsequently unable to maintain that citizen support. The results of this investigation could become important input for those responsible for communications in the Presidency of the Republic or other government agencies.

El objetivo del presente estudio fue explorar la relación entre el Crecimiento Postraumático (CPT) y el recuerdo de la Crianza Basada en Fortalezas (CBF) en víctimas adultas del Fenómeno del Niño en el año 2017; pertenecientes a los distritos de San Juan de Lurigancho, Churin, Oyon, Huaral, Barranca y Quilmaná. Para ello, se contó con la participación voluntaria de 611 damnificados cuyas edades oscilaron entre los 18 y 60 años. Se aplicó de manera presencial el Inventario de Crecimiento Postraumático (PTGI; Tedeschi & Calhoun, 1996) y el Cuestionario de Crianza Basada en Fortalezas (SBP; Waters, 2015), siendo este último adaptado a una visión en retrospectiva y traducido al idioma español. Los resultados de los análisis psicométricos mostraron que ambas escalas cuentan con una consistencia interna adecuada. Por su parte, las correlaciones y el modelo de regresión señalaron que la edad y el sexo son antecedentes potentes del crecimiento postraumático en los afectados por los huaycos. Por último, confirmaron que el uso de las fortalezas, potencializadas durante la crianza y mantenidas a lo largo del tiempo a través del recuerdo, reportan una relación positiva y un grado de prección significativo del CPT y todas sus dimensiones. Pues, esta modalidad de crianza refuerza una serie de cualidades positivas que se consolidan como parte de la propia identidad, las cuales son utilizadas de manera natural y efectiva como recursos protectores ante la adversidad. / The aim of this study was to explore the relation of Post-traumatic Growth (PTG) and Strength Based Parenting (SBP), after the severe mudslides of the 2017 El Niño Phenomenon in San Juan de Lurigancho, Churin, Oyon, Huaral, Barranca and Quilmaná. For this, there was the voluntary participation of 611 victims whose ages ranged from 18 and 60 years old. The Post-Traumatic Growth Inventory (PTGI; Tedeschi & Calhoun, 1996) and the Strengths-Based Parenting Questionnaire were applied, the latter being adapted in retrospect and translated into the Spanish language. The results of the psychometric analyzes showed that both scales have adequate internal consistency. On the other hand, the correlations and the regression model indicated that age and sex are potent antecedents of post-traumatic growth in those affected by the mudslides. Finally, the results confirmed that the use of the strengths, potentialized during the parenting and maintained over the time through the memory, report positive relationship and a significant degree of prediction of the PTG and all its dimensions. Well, this type of parenting reinforces during the first years of life a series of positive qualities that make up the own identity, which are used naturally and effectively as protective resources against adversity over time.

En el año 2017, Perú sufrió los impactos de El Niño costero, lo que afectó gravemente los ecosistemas y las poblaciones. Una de las zonas afectadas por este evento fue el distrito de Lunahuaná, en la región Lima, que presenta una alto riesgo a eventos climáticos extremos como El Niño. En el contexto del cambio climático, es relevante cuestionarse ¿cómo se comportan los actores sociales en localidades ribereñas como Lunahuaná frente a los impactos de El Niño a partir de su percepción sobre los eventos climáticos extremos? Desde el estudio de las percepciones y acciones frente al impacto del evento El Niño costero 2017 en las actividades turísticas en Lunahuaná, la investigación busca comprender la interacción entre las percepciones y el comportamiento humano frente al riesgo climático. La principal metodología fue la aplicación de entrevistas a profundidad, y los resultados muestran que los actores no se percibían en una situación de riesgo climático, lo que influyó en la escasa toma de acciones de reducción de riesgo y protección a eventos climáticos extremos. / In 2017, Peru suffered from the impacts of the coastal El Niño, which seriously affected ecosystems and populations. One of the areas affected by this event was the district of Lunahuana in the Lima region, which presents high risk of extreme weather events such as El Niño. In the context of climate change, it is relevant to ask how social actors in riverside towns such as Lunahuana behave in the face of the impacts of El Niño, given their perception of extreme climate events. Based on study of perceptions and actions regarding the impacts of the 2017 coastal El Niño event on tourism activities in Lunahuana, this research seeks to understand the interaction between perceptions and human behavior regarding climate risk. The main research methodology was the application of in-depth interviews, and the results show that actors did not perceive themselves to be in a situation of climate risk, which influenced the limited actions taken to reduce risk and protect against extreme climate events.

The Peruvian anchoveta fishery was for nearly 60 years characterized by the unsustainable dynamics of open access resource pools. This thesis investigates whether the 2009 Peruvian Legislative Decree 1084 on Individual Vessel Quotas (IVQ's) is an effective response to the industrial overcapacity and race-to-fish problems that threatened the environment before its implementation. It employs Common-Pool Resource theory to assess the impact of the new IVQ scheme on collective dynamics, and Ribot and Peluso's access theory (2009) to elucidate evolving power relations in the fishery. In this framework, DL1084 is evaluated as a regulatory instrument, as a lens on fisheries governance in Peru, and as a source of insight into how environmental impact serves in developing regulations of natural resource exploitation. A triangulated mixed-method design is employed: (1) a two-stream literature review of fisheries management and of the fishery's political ecology; (2) a quantitative analysis of daily state-published landings reports; and (3) seven in-depth intensive interviews with key actors in the fishery, conducted in Peru over two field-trips of approximately 2 months in total. Results indicate that although IVQ's supported existing trends towards large-scale economic efficiency and altered extreme competitive strategies previously associated with open access, fishing companies have built larger ships, favour bigger catches and still concentrate fishing effort around a given annual peak. Meanwhile, capacity has again increased in the unregulated artisanal fishery sector. DL1084 appears to reflect a broader process of growing private sector involvement in managing the fishery, made official by its institutionalization of market self-regulation. Ultimately, it evidences deep structure and capacity limitations in the state's ability to govern marine resources. The law was nevertheless seen as a landmark for the environmental legal process in Peru and an opportunity for reform. This thesis suggests that studying such legislations can provide insight into state identity and the evolving relationship between a nation and its geography. / Durante casi 60 años, la pesquería peruana de anchoveta estaba caracterizada por las dinámicas insostenibles de la explotación de recursos de propiedad común en situación de acceso abierto. Esta tesis investiga si el Decreto Legislativo Peruano 1084 (DL1084) sobre Límites Máximos de Captura por Embarcación (LMCE) es una respuesta efectiva a los problemas de sobrecapacidad industrial y de carrera por el recurso que amenazaban el ambiente antes de su aplicación en 2009. Se basa en la teoría de los Recursos de Propiedad Común (Common-Pool Resource theory) para evaluar el impacto del nuevo modelo de gestión por LMCE sobre las dinámicas colectivas, y en la teoría del Acceso de Ribot y Peluso (2009) para trazar la evolución de las relaciones de poder en la pesquería. En este marco, el DL1084 es evaluado como herramienta regulatoria, como lente sobre la gobernanza pesquera en el Perú y como reflejo del proceso por el cual el impacto ambiental sirve como base para el desarrollo de regulaciones sobre el acceso a recursos naturales. Sigue un diseño triangulado de métodos combinados: (1) una revisión de literatura en dos ramas de la gestión de pesquería como campo general y de la ecología política de la pesquería de anchoveta; (2) un análisis cuantitativo de los informes diarios de desembarques publicados por el estado (IMARPE); y (3) siete entrevistas intensivas de fondo con actores claves en la pesquería, realizadas en Perú durante dos visitas de aproximadamente dos meses en total. Los resultados indican que a pesar de que los LMCE soportaron una tendencia existente hacia una eficiencia económica de mayor escala y alteraron las estrategias competitivas extremas asociadas con el acceso abierto, las empresas pesqueras han construido embarcaciones más grandes, favorecen capturas de mayor tamaño y todavía concentran su esfuerzo pesquero alrededor de un pico anual de abundancia. En paralelo, ha aumentado la capacidad de captura en el sector artesanal, el cual no cuenta con límites de captura. El DL1084 aparece como parte de un proceso más general de creciente involucramiento del sector privado en el manejo de la pesquería, haciéndolo oficial por su misma institucionalización de la autorregulación del mercado. Por último, pone en evidencia profundas limitaciones de estructura y de capacidad en el estado en cuanto a cómo gobierna los recursos marinos. La ley ha sin embargo sido vista como un precedente importante para el proceso legislativo ambiental en el Perú así como una oportunidad para impulsar otras reformas. Esta tesis sugiere que el estudio de tales legislaciones puede ofrecer una mirada sobre los procesos de formación de la identidad de un estado y sobre la evolución de la relación entre una nación y su geografía.

No description available.

Em escalas interanuais a advecção de calor, sal e nutrientes pode afetar a produtividade primária. Pode-se citar a Circulação de Revolvimento Meridional (MOC) no impacto da concentração de clorofila. Neste estudo, a partir do método Multidimensional Empirical Mode Decomposition foram obtidos tendências decadais de PAR, nitrato integrado na coluna d\'água, concentração de clorofila e fluxo de volume da MOC. Em variações de baixa frequência há uma relação entre o transporte de volume da MOC com o nitrato integrado na coluna d\'água no Atlântico Sul, e consequentemente, na concentração de clorofila. Dois possíveis cenários foram identificados sobre o efeito da MOC no nitrato integrado e na concentração de clorofila. O cenário 1 apresenta uma relação direta no sistema MOC-nitrato integrado-concentração de clorofila, enquanto o efeito do cenário 2 é indireto, com a MOC afetando outras variáveis que perturbam o sistema. Neste estudo também foi analisado a influência de teleconexões atmosféricas na MOC do Atlântico Sul. Foi achado indícios da influência da Oscilação Antártica na MOC do Atlântico Sul em escalas decadais. Conclui-se que variações de baixa frequência no fluxo de volume da MOC alteram o padrão espaço-temporal da concentração de clorofila no Atlântico Sul. / On interannual timescales the advection of heat, salt and nutrients can affect the primary production. The influence of the Meridional Overturning Circulation (MOC) over the chlorophyll concentration can be mentioned. In this study, decadal trends of PAR, integrated nitrate over the water column, chlorophyll and volume flux of the MOC were obtained using the Multidimensional Empirical Mode Decomposition method. On low frequency variations there is a relationship between the MOC volume transport with integrated nitrate over the water column in the South Atlantic, and therefore, on chlorophyll concentration. Two scenarios were identified as possible mechanisms of influence of the MOC over integrated nitrate and chlorophyll concentrations. Scenario 1 presents a direct relationship on the system MOC-integrated nitrate-chlorophyll concentration, while scenario 2 has an indirect effect, with the MOC affecting other variables that disturb the system. In this study the influence of atmospheric teleconnections on the South Atlantic MOC were also investigated. It was found evidence that the Antarctic Oscillation can affect the South Atlantic MOC on decadal timescales. It was concluded that low frequency variability on the volume flux of the MOC can alter the spatiotemporal pattern of the chlorophyll concentration on the South Atlantic.

Nas últimas décadas, particularmente desde a década de 1970, testemunhou-se um rápido recuo das geleiras em várias partes dos Andes tropicais. Uma tendência de aquecimento foi observada na região durante o mesmo período, com um hiato recente desde no início de 2010. No entanto, este hiato pode não ser o principal fator a influenciar as observações de aquecimento e recuo das geleiras em altitudes elevadas nos Andes tropicais. Com o surgimento de imagens de alta resolução espacial e espectral, e de modelos digitais de elevação (MDE) de alta resolução, agora é possível compreender as mudanças multitemporais das geleiras, o que era difícil de realizar utilizando as técnicas tradicionais e os dados de baixa resolução. Neste trabalho foram calculadas as variações da linha de neve das geleiras selecionadas ao longo dos Andes tropicais desde o início de 1980. A linha de neve máxima observada durante a estação seca (inverno austral) nos trópicos pode ser considerada como equivalente à linha de equilíbrio que separa a zona de acumulação da zona de ablação. A fim de reduzir o erro na estimativa da linha de neve foram consideradas somente as geleiras com declividades menores que 20o. Dependendo da região estudada e da presença de cobertura de nuvens, foram selecionadas imagens de várias fontes. As imagens da série Landsat (MSS, TM, ETM+ e OLI), EO1 OLI, ASTER e IRS LISS III foram usadas junto com MDE do ASTER GDEM-v2. Três bandas espectrais (TM5 - infravermelho médio, TM4- infravermelho próximo e TM2 - verde) foram utilizadas para calcular a linha de neve durante a estação seca, aplicando limiares adequados para TM4 e TM2. Os conjuntos de dados meteorológicos de várias fontes também foram analisados para observar as mudanças na precipitação, na temperatura e na umidade que influenciam os parâmetros glaciológicos como: o balanço de massa e a linha de equilíbrio. Geleiras representativas nos trópicos internos e trópicos externos foram consideradas separadamente dentro de um novo quadro, que foi baseado na precipitação, umidade e condições de temperatura ao longo da América do Sul. Neste âmbito, os Andes tropicais são classificados em trópicos internos, trópicos externos úmidos do norte, trópicos externos úmidos do sul e os trópicos externos secos. O Vulcão Cotopaxi no Equador (trópicos internos), o Nevado Caullaraju-Pastoruri que é uma geleira na Cordilheira Branca no Peru (trópicos externos úmidos do norte), o Nevado Cololo na Cordilheira Apolobamba na Bolívia (trópicos externos úmidos do sul), o Nevado Coropuna na Cordilheira Ampato no Peru e o Nevado Sajama na Cordilheira Ocidental da Bolívia (trópicos externos secos) são as geleiras representativas de cada grupo consideradas neste estudo. As geleiras tropicais nos trópicos internos, especialmente as situadas perto da Zona de Convergência Intertropicais (ZCIT), são mais vulneráveis a aumentos na temperatura e menos sensíveis a variações na precipitação. Em contraste, as geleiras nos trópicos externos respondem à variabilidade de precipitação muito rapidamente em comparação com a variação de temperatura, particularmente quando se deslocam para as regiões subtropicais. A dependência do balanço de massa sobre as características de sublimação também aumenta a partir dos trópicos internos para os trópicos externos. As condições de aquecimento, com maior umidade, tendem a aumentar a perda de massa por causa do derretimento em vez da sublimação. A elevação da umidade nos trópicos externos pode alterar as geleiras dominadas pela sublimação (nos trópicos externos e subtrópicos) e para as geleiras dominadas por derretimento. Observa-se que as geleiras próximas da ZCIT (trópicos internos e trópicosexternos úmidos do sul) estão recuando mais rapidamente como uma resposta ao aquecimento global, enquanto que as geleiras nos trópicos externos úmidos do norte e trópicos externos secos mostraram recuo relativamente mais lento. Possivelmente isso pode ser devido à ocorrência de fases frias do El Niño - Oscilação Sul (ENOS) conjuntamente com a Oscilação Decenal do Pacífico (ODP). As anomalias observadas nas variáveis meteorológicas seguem os padrões de ODP e as variações anuais de linha de neve seguem eventos de El Niño particularmente na fase ODP quente. No entanto, uma forte correlação entre as variações da linha de neve e dos fenômenos ENOS (e ODP) não está estabelecida. As geleiras do Equador mostram menos retração em resposta à tendência de aquecimento se comparadas às observações feitas por outros pesquisadores na Colômbia e na Venezuela, provavelmente devido à grande altitude das geleiras equatorianas. Em poucas palavras, as geleiras menores e em baixas altitudes nos trópicos internos e trópicos externos úmidos do sul estão desaparecendo mais rapidamente do que outras geleiras nos Andes tropicais. Também se observou neste estudo a existência de uma propriedade direcional no recuo das geleiras, o que não se observou em quaisquer outros estudos recentes. As geleiras nas cordilheiras leste do Peru e da Bolívia, que alimentam muitos rios nos lados leste das cordilheiras orientais, estão recuando do que aquelas geleiras situadas nas encostas ocidentais dos Andes tropicais. / Recent decades, particularly since the late 1970s, witnessed a rapid retreat of glaciers in many parts of the tropical Andes. A warming trend is observed in this region during the same period, with a recent hiatus since the early 2010s. However, this hiatus is observed to have not influenced the retreat of high elevation glaciers in the tropical Andes. Due to the emergence of high spatial and spectral resolution images and high quality digital elevation models (DEM), it is now possible to understand the multi-temporal glacier changes compared with the techniques that existed a few decades before. We calculated the snowline variations of selected glaciers along the tropical Andes since the early 1980s. The maximum snowline observed during the dry season (austral winter) in the tropics can be considered as nearly equivalent to the equilibrium line that separates the accumulation zone from the ablation zone. In order to reduce the error in the estimated snowline, glaciers with slopes < 20o only were considered in this research. Depending on the study region and the presence of cloud cover, images from multiple sources were selected. Landsat series (MSS, TM, ETM+, and OLI), EO1 OLI, ASTER, and IRS LISS III images were used along with digital elevation models (DEM) from ASTER GDEM-v2. Three wavebands (TM5 - Middle Infrared, TM4 - Near Infrared, and TM2 - Green) were used to calculate the dry season snowline, after applying suitable threshold values to TM4 and TM2. Meteorological datasets from multiple sources were also analysed to observe the changes in precipitation, temperature, and humidity that influence key glaciological parameters such as the mass balance and the equilibrium line. Representative glaciers in the inner and the outer tropical Andes were considered separately within a new framework, which is based on the precipitation, humidity, and temperature conditions along the South America. In this framework, tropical Andes are classified in to inner tropics, northern wet outer tropics, southern wet outer tropics, and dry outer tropics. Cotopaxi ice-covered volcano, Ecuador (inner tropics), Nevado Caullaraju-Pastoruri Glacier, Cordillera Blanca, Peru (northern wet outer tropics), Nevado Cololo, Cordillera Apolobamba, Bolivia (southern wet outer tropics), and Nevado Coropuna, Cordillera Ampato Peru and Nevado Sajama, Cordillera Occidental, Bolivia (dry outer tropics) are the representative glaciers in each group considered in this study. Inner tropical glaciers, particularly those situated near the January Intertropical Convergence Zone (ITCZ), are more vulnerable to increases in temperature and these glaciers are less sensitive to variations in precipitation. In contrast, outer tropical glaciers respond to precipitation variability very rapidly in comparison with the temperature variability, particularly when moving towards the subtropics. Mass balance dependency on sublimation characteristics also increases from the inner tropics to the outer tropics. Warming conditions with higher humidity tends to enhance mass loss due to melting rather than sublimation. Increased humidity observed in the outer tropics may change the sublimation dominated glaciers in the outer tropics and subtropics to melting dominated ones in the future. It is observed that the glaciers above and near the January ITCZ (inner tropics and southern wet outer tropics) are retreating faster as a response to global warming, whereas the glaciers in the northern wet outer tropics and dry outer tropics show relatively slower retreat. This can be possibly due to the occurrence of cold phases of El Niño-Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO) together. The observed anomalies in the meteorological variables slightly follow PDO patterns and the variations in annual snowlines follows El Niño events, particularly when in phase with warm PDO. However, a strong correlation between snowline variations and ENSO (and PDO) is not established. Mountain glaciers in Ecuador show less retreat in response to the warming trend compared with observations done by other researchers in Colombia and Venezuela, probably due to very high altitude of the Ecuadorean glaciers. In a nutshell, smaller glaciers at lower altitudes in the inner tropics and the southern wet outer tropics are disappearing faster than other glaciers in the tropical Andes. Another observation made in this study is the directional property of glacier retreat, which was not covered in any other recent studies. Those glaciers on the eastern cordilleras of Peru and Bolivia, which feed many rivers on the eastern sides of the eastern cordilleras, are retreating faster than those glaciers situated on the western sides.

Ocean tides worldwide have exhibited secular changes in the past century, simultaneous with a global secular rise in mean sea level (MSL). The combination of these two factors contributes to higher water levels, and may increase threats to coastal regions and populations over the next century. Equally as important as these long-term changes are the short-term fluctuations in sea levels and tidal properties. These fluctuations may interact to yield locally extreme water level events, especially when combined with storm surge. This study, presented in three parts, examines the relationships between tidal anomalies and MSL anomalies on yearly and monthly timescales, with a goal of diagnosing dynamical factors that may influence the long-term evolution of tides in the Pacific Ocean. Correlations between yearly averaged properties are denoted tidal anomaly trends (TATs), and will be used to explore interannual behavior. Correlations of monthly averaged properties are denoted seasonal tidal anomaly trends (STATs), and are used to examine seasonal behavior. Four tidal constituents are analyzed: the two largest semidiurnal (twice daily) constituents, M2 and S2, and the two largest diurnal (once daily) constituents, K1 and O1. Part I surveys TATs and STATs at 153 Pacific Ocean tide gauges, and discusses regional patterns within the entire Pacific Ocean. TATs with statistically significant relations between MSL and amplitudes (A-TATs) are seen at 89% of all gauges; 92 gauges for M2, 66 for S2, 82 for K1, and 59 for O1. TATs with statistically significant relations between tidal phase (the relative timing of high water of the tide) and MSL (P-TATs) are observed at 55 gauges for M2, 47 for S2, 42 for K1, and 61 for O1. Significant seasonal variations (STATs) are observed at about a third of all gauges, with the largest concentration in Southeast Asia. The effect of combined A-TATs was also considered. At selected stations, observed tidal sensitivity with MSL was extrapolated forward in time to the predicted sea level in 2100. Results suggest that stations with large positive combined A-TATs produce total water levels that are greater than those predicted by an increase in MSL alone, increasing the chances of high-water events. Conversely, negative correlation between sea level and tidal properties may mitigate somewhat against sea level rise; changes in total water levels in 2100 at stations with a negative combined A-TAT are less than that predicted by MSL rise alone. Climate change scenarios that take into account greater increases in MSL due to increased Antarctic ice melt show larger changes in total water levels over the same time period. Part II examines the mechanisms behind the yearly (TAT) variability in the Western Tropical Pacific Ocean. Significant amplitude TATs are found at more than half of 26 gauges for each of the two strongest tidal constituents, K1 (diurnal) and M2 (semidiurnal). For the lesser constituents analyzed (O1 and S2), significant trends are observed at ten gauges. Frictional mechanisms related to the El Nino Southern Oscillation (ENSO) are found to be important in influencing tides in the Western Pacific, as well as resonant triad interactions, a nonlinear coupling that exchanges energy between the M2, K1, and O1 tides. Both of these factors contribute to the observed tidal variability in the Solomon Sea region. Part III analyzes the seasonal behavior of tides (STATs) at twenty tide gauges in the Southeast Asian waters, which exhibit variation by 10-30% of mean tidal amplitudes. A barotropic ocean tide model that considers the seasonal effects of MSL, stratification, and geostrophic and Ekman velocity is used to explain the observed seasonal variability in tides due to variations in monsoon-influenced climate forcing, with successful results at about half of all gauges. The observed changes in tides are best explained by the influence of non-tidal velocities (geostrophic and Ekman), though the effect of changing stratification is also an important secondary causative mechanism. From the results of these surveys and investigations, it is concluded that short-term fluctuations in MSL and tidal properties at multiple time scales may be as important in determining the state of future water levels as the long-term trends. Global explanations for the observed tidal behavior have not been found in this study; however, significant regional explanations are found at the yearly time scale in the Solomon Sea, and at the seasonal time scale in Southeast Asia. It is likely that tidal sensitivity to annual and seasonal variations in MSL at other locations also are driven by locally specific processes, rather than factors with basin-wide coherence.

Since Galileo Galilei invented the first thermometer, researchers have tried to understand the complex dynamics of ocean and atmosphere by means of scientific methods. They observe nature and formulate theories about the climate system. Since some decades powerful computers are capable to simulate the past and future evolution of climate.<br><br> Time series analysis tries to link the observed data to the computer models: Using statistical methods, one estimates characteristic properties of the underlying climatological processes that in turn can enter the models. The quality of an estimation is evaluated by means of error bars and significance testing. On the one hand, such a test should be capable to detect interesting features, i.e. be sensitive. On the other hand, it should be robust and sort out false positive results, i.e. be specific. <br><br> This thesis mainly aims to contribute to methodological questions of time series analysis with a focus on sensitivity and specificity and to apply the investigated methods to recent climatological problems. <br><br> First, the inference of long-range correlations by means of Detrended Fluctuation Analysis (DFA) is studied. It is argued that power-law scaling of the fluctuation function and thus long-memory may not be assumed a priori but have to be established. This requires to investigate the local slopes of the fluctuation function. The variability characteristic for stochastic processes is accounted for by calculating empirical confidence regions. The comparison of a long-memory with a short-memory model shows that the inference of long-range correlations from a finite amount of data by means of DFA is not specific. When aiming to infer short memory by means of DFA, a local slope larger than $alpha=0.5$ for large scales does not necessarily imply long-memory. Also, a finite scaling of the autocorrelation function is shifted to larger scales in the fluctuation function. It turns out that long-range correlations cannot be concluded unambiguously from the DFA results for the Prague temperature data set. <br><br> In the second part of the thesis, an equivalence class of nonstationary Gaussian stochastic processes is defined in the wavelet domain. These processes are characterized by means of wavelet multipliers and exhibit well defined time dependent spectral properties; they allow one to generate realizations of any nonstationary Gaussian process. The dependency of the realizations on the wavelets used for the generation is studied, bias and variance of the wavelet sample spectrum are calculated. To overcome the difficulties of multiple testing, an areawise significance test is developed and compared to the conventional pointwise test in terms of sensitivity and specificity. Applications to Climatological and Hydrological questions are presented. The thesis at hand mainly aims to contribute to methodological questions of time series analysis and to apply the investigated methods to recent climatological problems. <br><br> In the last part, the coupling between El Nino/Southern Oscillation (ENSO) and the Indian Monsoon on inter-annual time scales is studied by means of Hilbert transformation and a curvature defined phase. This method allows one to investigate the relation of two oscillating systems with respect to their phases, independently of their amplitudes. The performance of the technique is evaluated using a toy model. From the data, distinct epochs are identified, especially two intervals of phase coherence, 1886-1908 and 1964-1980, confirming earlier findings from a new point of view. A significance test of high specificity corroborates these results. Also so far unknown periods of coupling invisible to linear methods are detected. These findings suggest that the decreasing correlation during the last decades might be partly inherent to the ENSO/Monsoon system. Finally, a possible interpretation of how volcanic radiative forcing could cause the coupling is outlined. / Seit der Erfindung des Thermometers durch Galileo Galilei versuchen Forscher mit naturwissenschaftlichen Methoden die komplexen Zusammenhänge in der Atmosphäre und den Ozeanen zu entschlüsseln. Sie beobachten die Natur und stellen Theorien über das Klimasystem auf. Seit wenigen Jahrzehnten werden sie dabei von immer leistungsfähigeren Computern unterstützt, die das Klima der Erdgeschichte und der nahen Zukunft simulieren. <br><br> Die Verbindung aus den Beobachtungen und den Modellen versucht die Zeitreihen­analyse herzustellen: Aus den Daten werden mit statistischen Methoden charak­teristische Eigenschaften der zugrundeliegenden klimatologischen Prozesse geschätzt, die dann in die Modelle einfliessen können. Die Bewertung solch einer Schätzung, die stets Messfehlern und Vereinfachungen des Modells unterworfen ist, erfolgt statistisch entweder mittels Konfidenzintervallen oder Signifikanztests. Solche Tests sollen auf der einen Seite charakteristische Eigenschaften in den Daten erkennen können, d.h. sie sollen sensitiv sein. Auf der anderen Seite sollen sie jedoch auch keine Eigenschaften vortäuschen, d.h. sie sollen spezifisch sein. Für die vertrauenswürdige Untermauerung einer Hypothese ist also ein spezifischer Test erforderlich. <br><br> Die vorliegende Arbeit untersucht verschiedene Methoden der Zeitreihenanalyse, erweitert sie gegebenenfalls und wendet sie auf typische klimatologische Frage­stellungen an. Besonderes Augenmerk wird dabei auf die Spezifizität der jeweiligen Methode gelegt; die Grenzen möglicher Folgerungen mittels Datenanalyse werden diskutiert.<br><br> Im ersten Teil der Arbeit wird studiert, wie und ob sich mithilfe der sogenannten trendbereinigenden Fluktuationsanalyse aus Temperaturzeitreihen ein sogenanntes langes Gedächtnis der zugrundeliegenden Prozesse herleiten lässt. Solch ein Gedächtnis bedeutet, dass der Prozess seine Vergangenheit nie vergisst, mit fundamentalen Auswirkungen auf die gesamte statistische Beurteilung des Klimasystems. Diese Arbeit konnte jedoch zeigen, dass die Analysemethode vollkommen unspezifisch ist und die Hypothese “Langes Gedächtnis” gar nicht abgelehnt werden kann. <br><br> Im zweiten Teil werden zunächst Mängel einer sehr populären Analysemethode, der sogenannten kontinuierlichen Waveletspetralanalyse diskutiert. Diese Methode schätzt die Variabilität eines Prozesses auf verschiedenen Schwingungsperioden zu bestimm­ten Zeiten. Ein wichtiger Nachteil der bisherigen Methodik sind auch hier unspezi­fische Signifikanztests. Ausgehend von der Diskussion wird eine Theorie der Wavelet­spektralanalyse entwickelt, die ein breites Feld an neuen Anwendungen öffnet. Darauf basierend werden spezifische Signifikanztests konstruiert.<br><br> Im letzten Teil der Arbeit wird der Einfluss des El Niño/Southern Oscillation Phäno­mens auf den Indischen Sommermonsun analysiert. Es wird untersucht, ob und wann die Oszillationen beider Phänomene synchron ablaufen. Dazu wird eine etablierte Methode für die speziellen Bedürfnisse der Analyse von typischerweise sehr unregel­mäßigen Klimadaten erweitert. Mittels eines spezifischen Signifikanztests konnten bisherige Ergebnisse mit erhöhter Genauigkeit bestätigt werden. Zusätzlich konnte diese Methode jedoch auch neue Kopplungsintervalle feststellen, die die Hypothese entkräften konnten, dass ein neuerliches Verschwinden der Kopplung ein beisspielloser Vorgang sei. Schliesslich wird eine Hypothese vorgestellt, wie vulkanische Aerosole die Kopplung beeinflussen könnten.

Comprendre les mécanismes moteurs et pouvoir anticiper l'impact environnemental du phénomène El Niño Oscillation Australe (ENOA) constituent des enjeux scientifiques et sociétaux de première importance, notamment pour les Pays Emergents. Dans cette thèse, nous avons documenté et contrasté la signature de différents types d'ENOA - dits canoniques et Modoki - pour plusieurs variables climatiques essentielles (température et salinité de surface, niveau de la mer, courant de surface, précipitation, vent de surface, ...), analysé la pertinence de la théorie dite de recharge / décharge, une des quatre théories majeures d'ENOA, à rendre compte ou non de la nature quasi oscillatoire de ces différents types et quantifié l'impact potentiel des modifications des caractéristiques majeures d'ENOA sur notre interprétation des tendances climatiques à 'long' terme pour ces variables climatiques essentielles.