STUDY OF THE EQUATORIAL ATLANTIC OCEAN MIXING LAYER USING A ONE-DIMENSIONAL TURBULENCE MODEL

The General Ocean Turbulence Model (GOTM) is applied to the diagnostic turbulence field of the mixing layer (ML) over the equatorial region of the Atlantic Ocean. Two situations were investigated: rainy and dry seasons, defined, respectively, by the presence of the intertropical convergence zone and by its northward displacement. Simulations were carried out using data from a PIRATA buoy located on the equator at 23 degrees W to compute surface turbulent fluxes and from the NASA/GEWEX Surface Radiation Budget Project to close the surface radiation balance. A data assimilation scheme was used as a surrogate for the physical effects not present in the one-dimensional model. In the rainy season, results show that the ML is shallower due to the weaker surface stress and stronger stable stratification; the maximum ML depth reached during this season is around 15 m, with an averaged diurnal variation of 7 m depth. In the dry season, the stronger surface stress and the enhanced surface heat balance components enable higher mechanical production of turbulent kinetic energy and, at night, the buoyancy acts also enhancing turbulence in the first meters of depth, characterizing a deeper ML, reaching around 60 m and presenting an average diurnal variation of 30 m.

DETECTABILITY AND ERROR ESTIMATION IN ORBITAL FITS OF RESONANT EXTRASOLAR PLANETS

We estimate the conditions for detectability of two planets in a 2/1 mean-motion resonance from radial velocity data, as a function of their masses, number of observations and the signal-to-noise ratio. Even for a data set of the order of 100 observations and standard deviations of the order of a few meters per second, we find that Jovian-size resonant planets are difficult to detect if the masses of the planets differ by a factor larger than similar to 4. This is consistent with the present population of real exosystems in the 2/1 commensurability, most of which have resonant pairs with similar minimum masses, and could indicate that many other resonant systems exist, but are currently beyond the detectability limit. Furthermore, we analyze the error distribution in masses and orbital elements of orbital fits from synthetic data sets for resonant planets in the 2/1 commensurability. For various mass ratios and number of data points we find that the eccentricity of the outer planet is systematically overestimated, although the inner planet`s eccentricity suffers a much smaller effect. If the initial conditions correspond to small-amplitude oscillations around stable apsidal corotation resonances, the amplitudes estimated from the orbital fits are biased toward larger amplitudes, in accordance to results found in real resonant extrasolar systems.

Desiccation tolerance in Pleurostima purpurea (Velloziaceae)

Previous works suggested that Pleurostima purpurea (Velloziaceae-Barbacenioideae) shows a remarkable capacity to endure desiccation of its vegetative tissues. P. purpurea occurs in monocotyledons mats on soil islands in the Pao de Acucar (Sugar Loaf) one of the most recognizable rock outcrops of the world, in Rio de Janeiro, southeastern Brazil. Mats of P. purpurea occur in cliffs by the sea some meters above the tidal zone. Although living in rock outcrops almost devoid of any soil cover, P. purpurea seems to occur preferably on less exposed rock faces and slightly shady sites. Usually, less extreme adaptations to drought would be expected in plants with the habitat preference of P. purpurea. Relying on this observation, we argue if a combination of different strategies of dealing with low water availability can be found in P. purpurea as on other desiccation tolerant angiosperms. This study aims to examine the occurrence of desiccation tolerant behavior in P. purpurea together with the expression of drought avoidance mechanisms during dehydration progression. For this, it was analyzed the gas exchanges, leaf pigments and relative leaf water content during desiccation and rehydration of cultivated mature individuals. P. purpurea behaved like typical drought avoiders under moderated drought condition with stomatal closure occurring around a relative leaf water content up to 90%. During this process, it was observed a delay in the leaf relative water content (RWC(leaf)) decrease comparing to the plant-soil relative water content (RWC(plant-soil)). As soil dehydration worsened, gas exchanges restrictions progressed until a lack of activity which characterizes anabiosis. The loss of chlorophyll occurs before the end of total dehydration, characterizing the presence of poikilochlorophylly. The chlorophyll degradation follows the RWC(leaf) decrease, which achieved the minimum average value of 17% without incurring in leaf abscission. The chlorophyll re-synthesis seems to start well after the full rehydration of the leaf. During all of this process, carotenoid content remained stable. These results are coherent with a combination of drought avoidance and desiccation tolerance in P. purpurea which seems to be coherent with the amplitude of water availability in the rock outcrop habitat where it occurs, suggesting that the periods of water availability are sufficiently long for the success of the costly desiccation tolerant behavior but too short to make a typical drought avoider species win the competition for exploring the rock outcrop substrate where P. purpurea occurs.

Exercise-induced plasticity of AMPA-type glutamate receptor subunits in the rat brain

The aim of this study was to analyze the plastic effects of moderate exercise upon the motor cortex (M1 and M2 areas), cerebellum (Cb), and striatum (CPu) of the rat brain This assessment was made by verifying the expression of AMPA type glutamate receptor subunits (GluR1 and GluR2/3) We used adult Wistar rats, divided into 5 groups based on duration of exercise training, namely 3 days (EX3), 7 days (EX7) 15 days (EX15) 30 days (EX30), and sedentary (S) The exercised animals were subjected to a treadmill exercise protocol at the speed of the 10 meters/min for 40 mm After exercise, the brains were subjected to immunohistochemistry and immunoblotting to analyze changes of GluR1 and GluR2/3, and plasma cortcosterone was measured by ELISA in order to verify potential stress induced by physical training Overall the results of immunohistochemistry and immunoblotting were similar and revealed that GluR subunits show distinct responses over the exercise periods and for the different structures analyzed In general, there was increased expression of GluR subunits after longer exercise periods (such as EX30) although some opposite effects were seen after short periods of exercise (Ex3) In a few cases biphasic patterns with decreases and subsequent increases of GluR expression were seen and may represent the outcome of exercise dependent, complex regulatory processes The data show that the protocol used was able to promote plastic GluR changes during exercise, suggesting a specific involvement of these receptors in exercise induced plasticity processes in the brain areas tested (C) 2010 Elsevier B V All rights reserved

Post-collisional lamprophyric event in Sierra Norte, Cordoba, Argentina: Mineralogical, geochemical and isotopic characteristics

Over 20 lamprophyre dykes, varying in width between a few centimeters and several meters, have been identified in central Sierra Norte - Eastern Pampean Ranges, Cordoba, Argentina. Their mineralogy and chemistry indicate that they are part of the calc-alkaline lamprophyres clan (CAL). They contain phenocrysts of magnesiohomblende +/- augite set in a groundmass of magnesiohornblende, calcic-plagioclase, alkali feldspar, and opaque minerals, which designate them as spessartite-type lamprophyres. Alteration products include chlorite, calcite and iron oxides after malfic phenocrysts, though some are partially replaced by actinolite. Feldspars are replaced by carbonate and clay minerals. The dykes are relatively primitive, and show restricted major element variation (SiO(2) 51.1-55.3 wt.%, Al(2)O(3) 12-16.6 wt.%, total alkalies 1.5-4.7 wt.%), high Mg# (55-77), high Cr contents (27-988 ppm) and moderate to high Ni contents (60-190 ppm). Lamprophyre LILE (e.g. Rb averages 110 ppm, Sr 211-387 ppm, Ba 203-452 ppm) are high relative to HFSE (e.g., Ta 0.2-1.6 ppm, Nb 4-11 ppm, Y 17-21 ppm), and are enriched in LREE (30-70 times chondrite). They are characterized by relatively high (208)Pb/(204)Pb (38.8-39.9), (207)Pb/(204)Pb(similar to 15.7), and (206)Pb/(204)Pb (18.7-20.1), combined with low (epsilon)epsilon(Nd) (-4.69 to -1.52) and a relative moderately high ((87)Sr/(86)Sr)(i) of 0.7055-0.7074. The Rb-Sr whole rock isochron indicates an Early Ordovician age of 485 +/- 25 Ma. The calculated T(DM) (1.7 Ga) suggests that these rocks appear to have originated from a reservoir that was created during a mantle metasomatism event related to the Pampean orogeny. The Sierra Norte lamprophyres show affinities with a subduction-related magma in an active continental margin. Their geochemical and isotopic features suggest a multicomponent source, composed of enriched mantle material variably contaminated by crustal components. The lamprophyric suite emplacement occurred at the dawning stage of the Pampean orogeny, in a regional post-collisional extensional setting developed in the Sierra Norte-Ambargasta batholith (SNAB) in Early Ordovician times. (C) 2008 Published by Elsevier Ltd.

THE SOUTHERN BRAZILIAN SHELF: GENERAL CHARACTERISTICS, QUATERNARY EVOLUTION AND SEDIMENT DISTRIBUTION

Extending from latitude 34 degrees S to 22 degrees S the Southern Brazilian shelf constitutes the only part of the Brazilian shelf with a subtropical to temperate environment. The studies on the different geological aspects of the area began in the 1960`s and have recently been reassessed after studies related to the determination of the Economic Exclusive Zone. In terms of morphology, the Southern Brazilian shelf may be divided into three sectors, the Sao Paulo Bight, the Florianopolis-Mostardas Sector and the Rio Grande Cone, characterized by conspicuous differences in terms of geological determining factors, bathymetry, declivities and the presence of canyons and channels. Despite the existence of hundreds of radiocarbon datings the sea level changes curve of southern Brazil during the Last Glacial Cycle is still a matter of debate. A recent controversy on the Middle and late Holocene sea level changes curve raised the question of the amplitude of the oscillations which occurred in the period. Also, a few but relatively consistent radiocarbon datings suggest the occurrence of a high sea level during Isotope Stage 3. In terms of sedimentary cover the Southern Brazilian shelf exhibits a very strong hydrodynamic control, both latitudinal and bathymetrical. The sector southward from 25 degrees S is characterized by the influence of the plume of water carrying sediments originating from the Rio de La Plata. Actually its presence is conspicuous up to 28 degrees S, with the area between this latitude and 25 degrees S constituting a transitional zone. In terms of bathymetry the outer shelf is marked by the ""floor-polisher"" effect of the Brazil Current, which is responsible for the maintenance of a relict facies in areas deeper than 100 meters.

Neopaleozoic striated surfaces in the granitic basement and clast pavement remains of Salto, SP

Near Guarau Ceramic, localized southwest of Salto city in the State of Sao Paulo, two granite outcrops, distant some tens of meters from each other, display Neopaleozoic striated surfaces. These surfaces are in contact with diamictites from the Itarare Subgroup. The striae correspond to sub parallel grooves with millimetric spacing and depth, oriented about N48E and dipping 12 degrees to 42 degrees towards SE. Observed features and association with diamictites indicate an origin by glacial abrasion due to ice movement from southeast towards northwest. About 1.8 km east of Salto, unconsolidated material containing flat-iron-shaped and striated clasts was found on top of granite outcrops, interpreted as clasts pavement remains.

Bullerförekomst vid sönderdelning av skogsbränsle

Syftet med denna studie är att öka kunskapen om bullerexponering för omgivning och förare vid sönderdelning av skogsbränsle till flis. Sammanlagt har sex fallstudier genomförts, tre skotare, två lastbilar och en mobil anläggning. Fallen har valts med syftet att representera olika typer av sönderdelningsekipage och teknik. Studierna har genomförts i Dalarnas, Stockholms och Gävleborgs län. Bullerexponering för omgivning och förare i samband med sönderdelning till flis har undersökts med föreskrivna metoder. Det är stora skillnader på bullerexponering för förarna av de olika ekipagen. En skotarförare har daglig bullerexponering under såväl insats- som gränsvärde. Två förare (en skotarförare och en lastbilsförare) överskred insatsvärde, men var under gränsvärdet. Övriga förares bullerexponering överskred gränsvärdet. Alla maskiner har bullernivåer över 40/45 dB(A) på 200 meters avstånd, vilket överstiger acceptabla nivåer dagtid för områden med fritidsbebyggelse och fritidsområden. Endast ett av ekipagen (en skotare) hade bullernivåer på 200 meters avstånd i nivå med riktlinjer för områden med bostäder för permanent boende.  Övriga ekipage hade högre värden. De slutsatser som kan göras från denna studie är: Merparten av förare vid sönderdelning av skogsbränsle till flis exponeras för dagliga bullernivåer som kräver åtgärder. Bullernivåerna varierar mellan olika typer av ekipage för sönderdelning av skogsbränsle till flis. Studerade ekipage har högre värden för buller på 200 meters avstånd till bostäder, arbetslokaler och friluftsområden än vad som rekommenderas.

Evaluation of a PVT Air Collector

Hybrid Photovoltaic Thermal (PVT) collectors are an emerging technology that combines PV and solar thermal systems in a single solar collector producing heat and electricity simultaneously. The focus of this thesis work is to evaluate the performance of unglazed open loop PVT air system integrated on a garage roof in Borlänge. As it is thought to have a significant potential for preheating ventilation of the building and improving the PV modules electrical efficiency. The performance evaluation is important to optimize the cooling strategy of the collector in order to enhance its electrical efficiency and maximize the production of thermal energy. The evaluation process involves monitoring the electrical and thermal energies for a certain period of time and investigating the cooling effect on the performance through controlling the air mass flow provided by a variable speed fan connected to the collector by an air distribution duct. The distribution duct transfers the heated outlet air from the collector to inside the building. The PVT air collector consists of 34 Solibro CIGS type PV modules (115 Wp for each module) which are roof integrated and have replaced the traditional roof material. The collector is oriented toward the south-west with a tilt of 29 ᵒ. The collector consists of 17 parallel air ducts formed between the PV modules and the insulated roof surface. Each air duct has a depth of 0.05 m, length of 2.38 m and width of 2.38 m. The air ducts are connected to each other through holes. The monitoring system is based on using T-type thermocouples to measure the relevant temperatures, air sensor to measure the air mass flow. These parameters are needed to calculate the thermal energy. The monitoring system contains also voltage dividers to measure the PV modules voltage and shunt resistance to measure the PV current, and AC energy meters which are needed to calculate the produced electrical energy. All signals recorded from the thermocouples, voltage dividers and shunt resistances are connected to data loggers. The strategy of cooling in this work was based on switching the fan on, only when the difference between the air duct temperature (under the middle of top of PV column) and the room temperature becomes higher than 5 °C. This strategy was effective in term of avoiding high electrical consumption by the fan, and it is recommended for further development. The temperature difference of 5 °C is the minimum value to compensate the heat losses in the collecting duct and distribution duct. The PVT air collector has an area of (Ac=32 m2), and air mass flow of 0.002 kg/s m2. The nominal output power of the collector is 4 kWppv (34 CIGS modules with 115 Wppvfor each module). The collector produces thermal output energy of 6.88 kWth/day (0.21 kWth/m2 day) and an electrical output energy of 13.46 kWhel/day (0.42 kWhel/m2 day) with cooling case. The PVT air collector has a daily thermal energy yield of 1.72 kWhth/kWppv, and a daily PV electrical energy yield of 3.36 kWhel /kWppv. The fan energy requirement in this case was 0.18 kWh/day which is very small compared to the electrical energy generated by the PV collector. The obtained thermal efficiency was 8 % which is small compared to the results reported in literature for PVT air collectors. The small thermal efficiency was due to small operating air mass flow. Therefore, the study suggests increasing the air mass flow by a factor of 25. The electrical efficiency was fluctuating around 14 %, which is higher than the theoretical efficiency of the PV modules, and this discrepancy was due to the poor method of recording the solar irradiance in the location. Due to shading effect, it was better to use more than one pyranometer.

Rekonstruktion av högsta kustlinjen (HK) med ny nationell höjdmodell (NNH) och LiDAR : En studie över västra Gästrikland

Denna studie har med hjälp av den nya nationella höjdmodellen (NNH), som bygger på LiDAR-teknik, försökt att i västra Gästrikland hitta och analysera de landskaps- och terrängformer som kallas för högsta kustlinjen (HK). Dessa forna strandlinjer efter den senaste istiden har undersökts tidigare i studieområdet med hjälp av avvägningsinstrument och genom jordprover på 11 lokaler åren 1925-1930 och på 8 lokaler åren 1954-1960. I studien har det undersökts hur väl det går att identifiera nya som äldre HK-lokaler, jämföra de äldre undersökningarna med resultatet från dagens moderna datorteknik. Genom att i ett GIS-program skapa en terrängskuggning av NNH, som innan leverans har särskilt mark- och vattenytan från vegetation och antropogena objekt, har höjder kunnat mätas längs HK-linjer med cirka 50 meters avstånd. På grund av den snabba landhöjningen de första 500 åren efter avsmältningen är de högst belägna spåren av stranderosion svårare att hitta än de lägre. Av de 25 lokaler som hittades och analyserades var 11 lokaler på platser som inte tidigare undersökts eller där HK tidigare inte har kunnat fastställas. Av de undersökta lokalerna klassades 10 som osäkra, 11 som halvskarpa, 3 som skarpa och 1 som ett HK-delta. Från söder mot norr i västra Gästrikland stiger HK med cirka 27 meter från 194 meter över havet till 221 meter över havet. Skillnaderna jämfört med de tidigare undersökningarna är cirka ±2 meter, med undantag för 4 lokaler med skillnader från cirka 4 meter över till cirka 10 meter under. Förutom de 25 lokalerna hittades 6 mycket osäkra lokaler där HK inte gick att fastställa. Av dessa ligger 5 i ett område nordost och öster om Hofors. LiDAR-tekniken ger kvantitativt fler lokaler i områden som eventuellt tidigare inte har kunnat besökas och är en mer tidseffektiv metod.

Estimating the Impact of Catastrophic Sea Level Rise in Maine

Maine's 3,500 miles of coastline is the longest coastline in the continental US. The goal of our study was to use GIS to estimate the impact future global sea level rise could potentially have on our state. We show the area of coastline and some of the economic and social impacts that would result from a rise of one meter and six meters. We used roads to estimate the impact on infrastructure and public building, including schools, libraries, hospitals, police and fire stations, as a measure of social impact. A sea level rise of six meters would result in a loss of over 650 km¬2 from coastal communities and cost the state of Maine over 3 million in repaving costs. Through our study, we hope coastal communities will be able to prepare for and react to the predicted changes in global sea level.

Wind Power Suitability Analysis for the Gulf of Maine

This map shows one option for a viable energy source that is clean, free and endless: wind power. This map shows that the coast of Maine has the potential space and wind speed to be a location for wind farms. Four NOAA buoys placed in different locations along the Maine coast are the source of the wind speed data for this project. The average wind speed of every ten minutes of every day for the year 2004 were averaged so that each buoy was represented by one number of wind speed measured in meters/ second. The values in between these four buoys were estimated, or interpolated, using ArcGIS. Other factors that I took into consideration during this lab were distance from airports (no wind farm can be with in a three mile radius of an airport ) and distance from counties (no one wants an offshore wind farm that obstructs their view). I calculated the most appropriate locations for a wind farm in ArcGIS, by adding these three layers. The final output shows an area along Mt. Desert to be the most appropriate for development.

Effective Data Management Enables Intelligent Utility Management

Instrumentation and automation plays a vital role to managing the water industry. These systems generate vast amounts of data that must be effectively managed in order to enable intelligent decision making. Time series data management software, commonly known as data historians are used for collecting and managing real-time (time series) information. More advanced software solutions provide a data infrastructure or utility wide Operations Data Management System (ODMS) that stores, manages, calculates, displays, shares, and integrates data from multiple disparate automation and business systems that are used daily in water utilities. These ODMS solutions are proven and have the ability to manage data from smart water meters to the collaboration of data across third party corporations. This paper focuses on practical, utility successes in the water industry where utility managers are leveraging instantaneous access to data from proven, commercial off-the-shelf ODMS solutions to enable better real-time decision making. Successes include saving $650,000 / year in water loss control, safeguarding water quality, saving millions of dollars in energy management and asset management. Immediate opportunities exist to integrate the research being done in academia with these ODMS solutions in the field and to leverage these successes to utilities around the world.

Variações das propriedades granulométricas dos sedimentos da Barreira Costeira da Pinheira (SC) durante a sua progradação no holoceno superior

A barreira costeira da Pinheira esta localizada no litoral Centro-Sul do estado de Santa Catarina. Sua rnorfologia e estratigrafia são típicas de uma barreira regressiva. Durante o Holoceno Superior (Últimos 5 ka), a barreira progradou cerca de 5.500 metros, a uma taxa media de 1 ,I mlano. Sua progradação foi determinada por um rebaixamento de aproximadamente 2 m do nível do mar e, principalmente, por uma expressivo aporte de sedimentos arenosos em seu sistema praial, provenientes da plataforma continental adjacente. Nos Últimos 3.500 metros de progradaHo da barreira, ocorridos nos Últimos 3.1 ka, cerca de 60 cordões de dunas frontais foram formados. O intervalo de tempo decorrido entre a formação de dois cordões sucessivos foi de aproximadamente 52 anos. O estudo das propriedades granulométricas do sistema praia-duna atual e de dois dos cordões antigos de dunas frontais, denominados cordões intermediArio e interno, e formados, respectivamente, há cerca de 1280 e 3140 anos AP, revelou que, nos Últimos 3 ka não ocorreram variações significativas destas propriedades. Esta não variação, no tempo, das propriedades granulométricas é atribuída a natureza policíclica do estoque de areia consumido na progradação da barreira e a sua manutenção como fonte de sedimentos durante a progradação, elou a uma relativa constância, nos últimos 3 ka, das condições dinâmicas gerais dos sistema praia-duna atual da enseada da Pinheira. O estudo comparativo entre os diferentes sub-ambientes, ou zonas do sistema praia-duna atual (face da praia, berma e duna frontal), mostrou que o desvio padrão e a assimetria são potencialmente importantes na distinção entre depdsitos eolicos (dunas frontais) e praiais (face da praia) da barreira.

A cultura do girassol como estratégia de competitividade para o agronegócio regional e nacional: importância para a agroenergia e a alimentação

Equacionar aquecimento global, escassez de alimentos e a crescente necessidade energética, tornou-se, atualmente, o grande desafio mundial. Existem diversas culturas agrícolas que podem ser exploradas de maneira estratégica e assim colaborar com a solução deste problema. Dentre elas, pode-se destacar a cultura do girassol (Helianthus Annuus). O girassol é uma das quatro maiores culturas oleaginosas no mundo, cultivado com sucesso nos cinco continentes, ocupando uma área de cultivo superior a 22 milhões de hectares. A participação do Brasil nesse montante é inferior a 1%. Acredita-se que essa pequena participação se deva a fatores sócio-econômicos e tecnológicos. Salienta-se, porém que o Brasil, por suas vantagens comparativas naturais e vantagens competitivas construídas possui condições favoráveis para seu desenvolvimento. Diante dos fatos, o objetivo deste trabalho é aprofundar o conhecimento da cadeia produtiva do girassol e através de sua utilização como estratégia de competitividade, avaliar de maneira sistêmica os impactos na matriz agrícola do País. Dentre as inúmeras vantagens dessa cultura, pode-se destacar: características agronômicas, físicas, químicas, organolépticas e versatilidade, que permitem a utilização e otimização dos fatores de produção já disponíveis; época de plantio (adaptabilidade a diferentes condições edafoclimáticas), podendo ser cultivado desde o Rio Grande do Sul até o Estado de Roraima; sistema radicular (raiz pode chegar a dois metros de profundidade), permitindo o melhor aproveitamento dos nutrientes e da água do solo e promovendo a reciclagem de nutrientes; alto teor de óleo nas sementes (30% a 55%) e; alto valor comercial dos co-produtos. Esse conjunto de características é analisado sob a ótica da teoria das vantagens competitivas e das economias de escala e escopo, demonstrando que com inteligência e pragmatismo, a cultura do girassol pode repetir, com vantagens, o que a soja representou para o agronegócio brasileiro.