Dynamics and Thermodynamics of the Arabian Sea Warm Pool

The present study examines the importance of low saline waters and resulting barrier layer in the dynamics of the ASWP using observational data.The oceanic general circulation models (OGCM) are very useful for exploring the processes responsible for the ASWP and their variability. The circulation and thermohaline structure stimulated by an OGCM changes a lot when the resolution is increased from mesoscale to macro scale. For a reasonable simulation of the ASWP, we must include the mesoscale turbulence in numerical models. Especially the SEAS is an eddy prominent region with a horizontal dimension of 100 to 500 km and vertical extent of hundred meters. These eddies may have an important role on the evolution of ASWP, which has not been explored so far.Most of the earlier studies in the SEAS showed that the heat buildup in the mixed layer during the pre-monsoon (March-May) is primarily driven by the surface heat flux through the ocean-atmosphere interface, while the 3-dimensional heat budget of the ML physical processes that are responsible for the formation of the ASWP are unknown. With this background the present thesis also examines the relative importance of mixed layer processes that lead to the formation of warm pool in the SEAS.

Characteristics of Arabian Sea mini warm pool and Indian summer monsoon

Arabian Sea Mini Warm Pool (ASMWP) is a part of the Indian Ocean Warm Pool and formed in the eastern Arabian Sea prior to the onset of the summer monsoon season. This warm pool attained its maximum intensity during the pre-monsoon season and dissipated with the commencement of summer monsoon. The main focus of the present work was on the triggering of the dissipation of this warm pool and its relation to the onset of summer monsoon over Kerala. This phenomenon was studied utilizing NCEP/NCAR (National Center for Environmental Prediction/National Center for Atmospheric and Research) re-analysis data, TRMM Micro wave Imager (TMI) and observational data. To define the ASMWP, sea surface temperature exceeding 30.25 C was taken as the criteria. The warm pool attained its maximum dimension and intensity nearly 2 weeks prior to the onset of summer monsoon over Kerala. Interestingly, the warm pool started its dissipation immediately after attaining its maximum core temperature. This information can be included in the present numerical models to enhance the prediction capability. It was also found that the extent and intensity of the ASMWP varied depending on the type of monsoon i.e., excess, normal, and deficient monsoon. Maximum core temperature and wide coverage of the warm pool observed during the excess monsoon years compared to normal and deficient monsoon years. The study also revealed a strong relationship between the salinity in the eastern Arabian Sea and the nature of the monsoon

Rock pool.

En las costas rocosas hay rocas que forman como piscinas que quedan cubiertas por las mareas que son las que llevan el oxígeno y los alimentos a docenas de diferentes animales y plantas. Muchos de esos animales se refugian bajo las rocas y entre las algas marinas a fin de que sus cuerpos no se sequen antes de que la marea suba de nuevo.

Large inert carbon pool in the terrestrial biosphere at the Last Glacial Maximum

During each of the late Pleistocene glacial–interglacial transitions, atmospheric carbon dioxide concentrations rose by almost 100 ppm. The sources of this carbon are unclear, and efforts to identify them are hampered by uncertainties in the magnitude of carbon reservoirs and fluxes under glacial conditions. Here we use oxygen isotope measurements from air trapped in ice cores and ocean carbon-cycle modelling to estimate terrestrial and oceanic gross primary productivity during the Last Glacial Maximum. We find that the rate of gross terrestrial primary production during the Last Glacial Maximum was about 40±10 Pg C yr−1, half that of the pre-industrial Holocene. Despite the low levels of photosynthesis, we estimate that the late glacial terrestrial biosphere contained only 330 Pg less carbon than pre-industrial levels. We infer that the area covered by carbon-rich but unproductive biomes such as tundra and cold steppes was significantly larger during the Last Glacial Maximum, consistent with palaeoecological data. Our data also indicate the presence of an inert carbon pool of 2,300 Pg C, about 700 Pg larger than the inert carbon locked in permafrost today. We suggest that the disappearance of this carbon pool at the end of the Last Glacial Maximum may have contributed to the deglacial rise in atmospheric carbon dioxide concentrations.

Processes driving intraseasonal displacements of the eastern edge of the warm pool: the contribution of westerly wind events

We investigate the processes responsible for the intraseasonal displacements of the eastern edge of the western Pacific warm pool (WPEE), which appear to play a role in the onset and development of El Niño events. We use 25 years of output from an ocean general circulation model experiment that is able to accurately capture the observed displacements of the WPEE, sea level anomalies, and upper ocean zonal currents at intraseasonal time scales in the western and central Pacific Ocean. Our results confirm that WPEE displacements driven by westerly wind events (WWEs) are largely controlled by zonal advection. This paper has also two novel findings: first, the zonal current anomalies responsible for the WPEE advection are driven primarily by local wind stress anomalies and not by intraseasonal wind-forced Kelvin waves as has been shown in most previous studies. Second, we find that intraseasonal WPEE fluctuations that are not related to WWEs are generally caused by intraseasonal variations in net heat flux, in contrast to interannual WPEE displacements that are largely driven by zonal advection. This study hence raises an interesting question: can surface heat flux-induced zonal WPEE motions contribute to El Niño–Southern Oscillation evolution, as WWEs have been shown to be able to do?

A trava bancária na recuperação judicial e o seu impacto nas formas de financiamento da empresa: uma análise através da teoria do “common pool assets” de Thomas H. Jackson

O objeto de estudo do presente trabalho é a Trava Bancária, mecanismo jurídico previsto no art. 49, § 3º da Lei de Falências e Recuperação Judicial de Empresas - LRF, por meio do qual dívidas contraídas pelas empresas junto às instituições financeiras são garantidas pela alienação fiduciária dos seus recebíveis. Serão analisadas as peculiaridades desse tipo de garantia fiduciária e, em especial, a prerrogativa que os credores detentores desse tipo de garantia possuem dentro dos procedimento de recuperação judicial de empresas, de não precisarem submeter seus créditos aos procedimentos concursais. Será feita uma análise para demonstrar que a manutenção da trava bancária diminui o valor de going concern da empresa em recuperação, pois a criação de um tipo de credor que é blindado quanto aos efeitos da recuperação judicial impede que essa mantenha-se como um procedimento concursal coletivo e compulsório, requisitos que são essenciais para incentivar os credores da empresa a trabalharem de forma conjunta, mantendo o valor de going concern da empresa recuperanda, com o objetivo de recuperar a empresa e saldarem seus créditos. Tem-se como objetivo demonstrar que, a existência da trava bancária na recuperação judicial, pode afetar negativamente o acesso das empresas ao financiamento por equity. Isto porque, os acionistas das empresas são os últimos da fila de credores a receberem caso a empresa entre em recuperação judicial, e, portanto, acredita-se que, ao saberem que existe um mecanismo que poderá inviabilizar a recuperação judicial das empresas em crise, atrapalhando sua geração de valor de going concern, é possível que investidores desistam de investir em empresas financiadas por dívidas garantidas pela alienação fiduciária de seus recebíveis, passando a ser essa uma variável levada em consideração quando da realização dos procedimentos de valuation para compra de participação acionária em empresas. Os pressupostos teóricos que serão utilizados para embasar a premissa de que a trava bancária gera impacto negativo no valor de going concern das empreas em crise, dificultando seu processo de recuperação, serão extraídos e elaborados a partir da Teoria da Common Pool Assets do autor norte-americano, Thomas H. Jackson. A relevância deste trabalho decorre da importância que o procedimento de recuperação judicial apresenta para as empresas em crise e para os seus credores, bem como a importância que esse tipo de procedimento adquiriu no País. Com efeito, desde a entrada em vigor da LRF no ordenamento jurídico brasileiro em 2005, cerca de 4 mil companhias já pediram recuperação judicial. Além disso, o trabalho mostra-se relevante por abordar questão relativa às formas de financiamento das empresas, assunto que tem reflexo no Custo Brasil e impacto direto no desenvolvimento da economia brasileiro.

Evolutionary transition to freshwater by ancestral marine palaemonids: evidence from osmoregulation in a tide pool shrimp

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Pool of Resistance Mechanisms to Glyphosate in Digitaria insularis

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Combined Pool/Bilateral Short-Term Hydrothermal Scheduling Model for Day-Ahead Energy Markets

This paper proposes a combined pool/bilateral short term hydrothermal scheduling model (PDC) for the context of the day-ahead energy markets. Some innovative aspects are introduced in the model, such as: i) the hydraulic generation is optimized through the opportunity cost function proposed; ii) there is no decoupling between physical and commercial dispatches, as is the case today in Brazil; iii) interrelationships between pool and bilateral markets are represented through a single optimization problem; iv) risk exposures related to future deficits are intrinsically mitigated; v) the model calculates spot prices in an hourly basis and the results show a coherent correlation between hydrological conditions and calculated prices. The proposed PDC model is solved by a primal-dual interior point method and is evaluated by simulations involving a test system. The results are focused on sensitivity analyses involving the parameters of the model, in such a way to emphasize its main modeling aspects. The results show that the proposed PDC provides a conceptual means for short term price formation for hydrothermal systems.

The Venomics of Bothrops alternatus is a Pool of Acidic Proteins with Predominant Hemorrhagic and Coagulopathic Activities

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Riffle and pool fish communities in a large stream of southeastern Brazil

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Removal of sunscreen compounds from swimming pool water using self-organized TiO2 nanotubular array electrodes

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)