Proteção em sistemas elétricos com geração distribuída utilizando a transformada wavelet

A typical electrical power system is characterized by centr alization of power gene- ration. However, with the restructuring of the electric sys tem, this topology is changing with the insertion of generators in parallel with the distri bution system (distributed gene- ration) that provides several benefits to be located near to e nergy consumers. Therefore, the integration of distributed generators, especially fro m renewable sources in the Brazi- lian system has been common every year. However, this new sys tem topology may result in new challenges in the field of the power system control, ope ration, and protection. One of the main problems related to the distributed generati on is the islanding formation, witch can result in safety risk to the people and to the power g rid. Among the several islanding protection techniques, passive techniques have low implementation cost and simplicity, requiring only voltage and current measuremen ts to detect system problems. This paper proposes a protection system based on the wavelet transform with overcur- rent and under/overvoltage functions as well as infomation of fault-induced transients in order to provide a fast detection and identification of fault s in the system. The propo- sed protection scheme was evaluated through simulation and experimental studies, with performance similar to the overcurrent and under/overvolt age conventional methods, but with the additional detection of the exact moment of the fault.

Age determination of North Atlantic sediment cores

Available overwash records from coastal barrier systems document significant variability in North Atlantic hurricane activity during the late Holocene. The same climate forcings that may have controlled cyclone activity over this interval (e.g., the West African Monsoon, El Niño-Southern Oscillation (ENSO)) show abrupt changes around 6000 yrs B.P., but most coastal sedimentary records do not span this time period. Establishing longer records is essential for understanding mid-Holocene patterns of storminess and their climatic drivers, which will lead to better forecasting of how climate change over the next century may affect tropical cyclone frequency and intensity. Storms are thought to be an important mechanism for transporting coarse sediment from shallow carbonate platforms to the deep-sea, and bank-edge sediments may offer an unexplored archive of long-term hurricane activity. Here, we develop this new approach, reconstructing more than 7000 years of North Atlantic hurricane variability using coarse-grained deposits in sediment cores from the leeward margin of the Great Bahama Bank. High energy event layers within the resulting archive are (1) broadly correlated throughout an offbank transect of multi-cores, (2) closely matched with historic hurricane events, and (3) synchronous with previous intervals of heightened North Atlantic hurricane activity in overwash reconstructions from Puerto Rico and elsewhere in the Bahamas. Lower storm frequency prior to 4400 yrs B.P. in our records suggests that precession and increased NH summer insolation may have greatly limited hurricane potential intensity, outweighing weakened ENSO and a stronger West African Monsoon-factors thought to be favorable for hurricane development.

Influence of Increased Human Presence in the Mills River Basin on Water Availability and Drought

Periods of drought and low streamflow can have profound impacts on both human and natural systems. People depend on a reliable source of water for numerous reasons including potable water supply and to produce economic value through agriculture or energy production. Aquatic ecosystems depend on water in addition to the economic benefits they provide to society through ecosystem services. Given that periods of low streamflow may become more extreme and frequent in the future, it is important to study the factors that control water availability during these times. In the absence of precipitation the slower hydrological response of groundwater systems will play an amplified role in water supply. Understanding the variability of the fraction of streamflow contribution from baseflow or groundwater during periods of drought provides insight into what future water availability may look like and how it can best be managed. The Mills River Basin in North Carolina is chosen as a case-study to test this understanding. First, obtaining a physically meaningful estimation of baseflow from USGS streamflow data via computerized hydrograph analysis techniques is carried out. Then applying a method of time series analysis including wavelet analysis can highlight signals of non-stationarity and evaluate the changes in variance required to better understand the natural variability of baseflow and low flows. In addition to natural variability, human influence must be taken into account in order to accurately assess how the combined system reacts to periods of low flow. Defining a combined demand that consists of both natural and human demand allows us to be more rigorous in assessing the level of sustainable use of a shared resource, in this case water. The analysis of baseflow variability can differ based on regional location and local hydrogeology, but it was found that baseflow varies from multiyear scales such as those associated with ENSO (3.5, 7 years) up to multi decadal time scales, but with most of the contributing variance coming from decadal or multiyear scales. It was also found that the behavior of baseflow and subsequently water availability depends a great deal on overall precipitation, the tracks of hurricanes or tropical storms and associated climate indices, as well as physiography and hydrogeology. Evaluating and utilizing the Duke Combined Hydrology Model (DCHM), reasonably accurate estimates of streamflow during periods of low flow were obtained in part due to the model’s ability to capture subsurface processes. Being able to accurately simulate streamflow levels and subsurface interactions during periods of drought can be very valuable to water suppliers, decision makers, and ultimately impact citizens. Knowledge of future droughts and periods of low flow in addition to tracking customer demand will allow for better management practices on the part of water suppliers such as knowing when they should withdraw more water during a surplus so that the level of stress on the system is minimized when there is not ample water supply.

Recent Changes in Central and Eastern Pacific El Niño

Recent research indicates that characteristics of El Niño and the Southern Oscillation (ENSO) have changed over the past several decades. Here, I examined different flavors of El Niño in the observational record and the recent changes in the character of El Niño events. The fundamental physical processes that drive ENSO were described and the Eastern Pacific (EP) and Central Pacific (CP) types or flavors of El Niño were defined. Using metrics from the peer-reviewed literature, I examined several historical data sets to interpret El Niño behavior from 1950-2010. A Monte Carlo Simulation was then applied to output from coupled model simulations to test the statistical significance of recent observations surrounding EP and CP El Niño. Results suggested that EP and CP El Niño had been occurring in a similar fashion over the past 60 years with natural variability, but no significant increase in CP El Niño behavior.

Dahlak coral d18O record (DGII) from the southern Red Sea

Coral palaeoclimatic studies are under way at many sites throughout the wet tropics. However, arid environments have received less attention. Here we report a high-resolution, 63 yr record of coral d18O and d13C extracted from a Porites colony from the Dahlak Archipelago, off the Eritrean coast, in the southern Red Sea. The annual cycles of the coral d18O and d13C are inversely related while their inter-annual variations show a strong positive correlation, with similar inter-decadal trends. Inter-annual variations in coral d18O show a relatively weak correlation with the southern Red Sea SST, but are strongly correlated with the Indian Ocean SST, especially on the decadal time-scale. The range of the inter-annual variations in the coral d18O is high compared to changes in local SST, due to the amplifying effect of simultaneous changes in water isotopic composition. Due to this amplification of the climate signal the coral provides a better indication of regional oceangraphic behaviour than the local SST record. The norrtheast monsoon signal in the coral d18O dominates the mean annual signal and shows the best correlation with the instrumental data sets. It appears that variations in the coral d18O are controlled mainly by variations in the intensity of surface water influx from the Indian Ocean to the Red Sea during the winter northeast monsoon. Of particular significance is that the decadal time-scale variations in the coral skeletal d18O are closely correlated with both the Indian Ocean SST and with variations in the Pacific-based Southern Oscillation index. That is, isotopically light coral skeleton, indicating strong NE monsoon Red Sea inflow, correlates with periods of high Indian Ocean SST and with predominantly negative (El Nino) phases of the Southern Oscillation. The simultaneous nature of inter-decadal changes in Asian monsoon and ENSO behaviour suggest pan-Indo-Pacific tropical climate reorganisation and evolution.

(Table 1) Age control points and of sediment core MD01-2444

The marine isotopic stage 3 (MIS3) at Ocean Drilling Program (ODP) Site 1060 (Gulf Stream) shows both sharp onset and end of interstadials, the existence of very short lived warm events during stadials, and points to differences in detail between the sea surface temperature (SST) record from the western North Atlantic and the atmospheric temperature record inferred from d18O in Greenland ice. Investigating MIS3 and obtaining comparable data from other locations appears crucial. The eastern Atlantic provides well-documented records of climate changes. We have selected a core from off Portugal and use it to examine Dansgaard/Oeschger events (D/O) at centennial-scale resolution (139 years on average between two data points). We have obtained a faunal data set for core MD01-2444, 37°N, 10°W, 2600 m water depth and use a group of species (Globigerina bulloides + Globigerinita glutinata) as a proxy of upwelling intensity driven by trade winds intensity changes. We tentatively relate the variation of this group to a North Atlantic Oscillation-like phenomenon (NAO) off Portugal. We observe that it resembles the rainfall index in the Caribbean as recorded at ODP Site 1002 (Cariaco Basin) which traces the Intertropical Convergence Zone (ITCZ) location through changes of terrigenous inputs. The driest intervals (ITZC to the south) at Site 1002 correspond to intervals of increased upwelling in MD01-2444 as well as the driest periods identified during stadials on similar cores in the area. Because the ITZC to the south is consistent with an El Niño-Southern Oscillation (ENSO+) situation, our study suggests a positive correlation between ENSO-like conditions and NAO-like conditions at a millennial timescale. During interstadial intervals when increased wetness over Cariaco is recorded (ITCZ to the north) and the upwelling in MD01-2444 is decreased, we see from both SSTs and faunal tropical indicators that MD01-2444 site is warm. In addition, interstadials are equally warm through each so-called Bond cycle. This contrasts with the Greenland Ice Core Project (GRIP) record where interstadial peaks are successively cooler through each Bond cycle. This record confirms a link between tropical climate linked to ITCZ position and the climate of southern Europe at millennial timescales, in spite of showing a very good correlation with polar latitudes (GRIP) through d18O on Globigerina bulloides. In addition, because the warmest SSTs and the d18O on G. bulloides are so remarkably different, our work points to changes in seasonality as a strong control over the climatic pattern of the North Atlantic area and the marked influence of winter conditions.

Stable oxygen isotope record of coral core RUS-95 from the Red Sea

A 245-year coral oxygen isotope record from the northern Red Sea (Ras Umm Sidd/Egypt, ~28°N) in bimonthly resolution is presented. The mean annual coral delta18O signal apparently reflects varying proportions of both sea surface temperature and delta18Oseawater variability. In conjunction with instrumental observations of climate the coral record suggests for interannual and longer timescales that colder periods are accompanied by more arid conditions in the northern Red Sea but increased rainfall in the southeastern Mediterranean, whereas warmer periods are accompanied by decreased rainfall in the latter and less arid conditions in the northern Red Sea. A ~70-year oscillation of probably North Atlantic origin dominates the coral time series. Interannual to interdecadal variability is correlated with instrumental indices of the North Atlantic Oscillation (NAO), the El Niño-Southern Oscillation (ENSO), and North Pacific climate variability. The results suggest that these modes contributed consistently to Middle East climate variability since at least 1750, preferentially at a period of ~5.7 years.

Oxygen isotopic measurements from Holcene of sediment core MD02-2529, tropical pacific

Changes in El Niño-Southern Oscillation (ENSO) variability are difficult to extract from paleoceanographic reconstructions because they are superimposed on changes in seasonal variability that modulate the first-order climate signal. Here we address this problem by reconstructing thermocline structure from a marine sediment core retrieved from the eastern equatorial Pacific. At the core location, changes in hydrologic parameters within the thermocline are linked to ENSO activity, with a reduced influence of seasonal variability compared to surface waters. We performed repeated isotopic analyses (d18O) on single specimens of the thermocline-dwelling planktonic foraminifera Neogloboquadrina dutertrei at several targeted time periods over the last 50 ka to extract the total thermocline variance, a parameter supposed to reveal changes in ENSO. No fundamental changes in amplitude and frequency of the events were detected despite differences in climatic background. However, our data suggest that long-term variations in the thermocline variability occurred over the last 50 ka, with the highest and lowest ENSO activities occurring during the last glacial period and the Last Glacial Maximum, respectively.

Planktic foraminifera abundances and winter SST reconstruction for sediment core SO90-39KG

The Indian winter monsoon (IWM) is a key component of the seasonally changing monsoon system that affects the densely populated regions of South Asia. Cold winds originating in high northern latitudes provide a link of continental-scale Northern Hemisphere climate to the tropics. Western Disturbances (WD) associated with the IWM play a critical role for the climate and hydrology in northern India and the western Himalaya region. It is vital to understand the mechanisms and teleconnections that influence IWM variability to better predict changes in future climate. Here we present a study of regionally calibrated winter (January) temperatures and according IWM intensities, based on a planktic foraminiferal record with biennial (2.55 years) resolution. Over the last ~250 years, IWM intensities gradually weakened, based on the long-term trend of reconstructed January temperatures. Furthermore, the results indicate that IWM is connected on interannual- to decadal time scales to climate variability of the tropical and extratropical Pacific, via El Niño Southern Oscillation (ENSO) and Pacific Decadal Oscillation (PDO). However, our findings suggest that this relationship appeared to begin to decouple since the beginning of the 20th century. Cross-spectral analysis revealed that several distinct decadal-scale phases of colder climate and accordingly more intense winter monsoon centered at the years ~1800, ~1890 and ~1930 can be linked to changes of the North Atlantic Oscillation (NAO).

(Table 2) Seasonal flux data and percentages of major bulk components of total flux at the mesotrophic sediment trap site CB from 1988 - 2012

A more than two-decadal sediment trap record from the Eastern Boundary Upwelling Ecosystem (EBUE) off Cape Blanc, Mauritania, is analysed with respect to deep ocean mass fluxes, flux components and their variability on seasonal to decadal timescales. The total mass flux revealed interannual fluctuations which were superimposed by fluctuations on decadal timescales. High winter fluxes of biogenic silica (BSi), used as a measure of marine production (mostly by diatoms) largely correspond to a positive North Atlantic Oscillation (NAO) index (December-March). However, this relationship is weak. The highest positive BSi anomaly was in winter 2004-2005 when the NAO was in a neutral state. More episodic BSi sedimentation events occurred in several summer seasons between 2001 and 2005, when the previous winter NAO was neutral or even negative. We suggest that distinct dust outbreaks and deposition in the surface ocean in winter and occasionally in summer/autumn enhanced particle sedimentation and carbon export on short timescales via the ballasting effect. Episodic perturbations of the marine carbon cycle by dust outbreaks (e.g. in 2005) might have weakened the relationships between fluxes and large-scale climatic oscillations. As phytoplankton biomass is high throughout the year, any dry (in winter) or wet (in summer) deposition of fine-grained dust particles is assumed to enhance the efficiency of the biological pump by incorporating dust into dense and fast settling organic-rich aggregates. A good correspondence between BSi and dust fluxes was observed for the dusty year 2005, following a period of rather dry conditions in the Sahara/Sahel region. Large changes of all bulk fluxes occurred during the strongest El Niño-Southern Oscillation (ENSO) in 1997-1999 where low fluxes were obtained for almost 1 year during the warm El Niño and high fluxes in the following cold La Niña phase. For decadal timescales, Bakun (1990) suggested an intensification of coastal upwelling due to increased winds (''Bakun upwelling intensification hypothesis''; Cropper et al., 2014) and global climate change. We did not observe an increase of any flux component off Cape Blanc during the past 2 and a half decades which might support this. Furthermore, fluxes of mineral dust did not show any positive or negative trends over time which might suggest enhanced desertification or ''Saharan greening'' during the last few decades.

Tracker : Applikationen som håller koll på din rörelse

Målet med det här arbetet har varit att ta fram en Androidapplikation som kan spåra användaren och ge information om hur användaren rört sig med tid, distans altitud och hastighet. Applikationen ska vara individuellt fungerande men det stora syftet är att den ska fungera som en av tre delar i en större applikation med fler funktioner för de som är ute i skogen och rör på sig. Då inte alla telefoner har en inbyggd stegräknare kommer en undersökning göras för att se vilken sensor som lämpar sig bäst för att räkna steg och sedan använda den i applikationen. Resultatet blev en fungerande applikation som spårar användaren med hjälp av GPS, räknar antalet steg med antingen den inbyggda stegräknaren eller med hjälp av gyroskopet som visade sig vara den mest lämpade sensorn att räkna steg med. Utöver det så presenteras information om tid, distans och vilken altitud användaren rört sig på. All information kan sparas och användaren kan scrolla i en lista med sparade rutter.

Attityder till teknikdidaktik i de tidigare årskurserna

Teknik är ett ämne som fortfarande är relativt nytt som obligatoriskt ämne i grundskolan. Ämnet anses av många som viktigt, men undersökningar från bl.a. skolinspektionen visar att det finns stora brister i hur tekniken behandlas inom grundskolan. I detta arbete ser jag över hur begreppet teknik definieras i undervisningssammanhang, dess historia som skolämne, samt tidigare forskning och insatser som gjorts för att stärka undervisningen i teknik. Därefter följer en enkätundersökning där jag har tillfrågat lärare på fyra grundskolor, med årskurserna f-6 (grundskolor med årskurs 7-9 har inte inkluderats), om deras egen inställning till teknik och vilken status de upplever att ämnet har på den skola de arbetar. Jag har valt att rikta mig mot denna målgrupp då jag upplever att teknikämnet är särskilt obehandlat i de allra tidigaste årskurserna. Resultatet av undersökningen analyseras i relation till den tidigare forskningen som jag har tagit upp. Min slutsats är att teknik till stor del undervisas enligt den traditionella praktiken som tidigare forskning beskriver, men att det varierar från skola till skola (samt från lärare till lärare på samma skola) hur ämnet prioriteras och praktiseras. Det verkar även finnas en stor kontrast i hur lärare i årskurs 1-3 respektive 4-6 ser på ämnet.

Den växande dagligvaruhandeln på internet : En fallstudie om MatHem i Sverige AB

Bakgrund Dagligvaruhandel på internet växer och efterfrågas från fler kunder än någonsin tidigare. De större aktörerna märker att efterfrågan finns och inser att de behöver utöka sina försäljningskanaler, samtidigt som de mindre företagen som varit med och bidragit till denna efterfrågan behöver arbeta för att hålla sina kunder lojala och inte förlora marknadsandelar när marknadssituationen förändras av de stora aktörerna. Den förändrade konkurrenssituationen innebär att företag behöver lägga större fokus på kunden genom strategi och framförallt uppbyggnaden av lojalitet. Syfte Syftet är att få en ökad kunskap om hur ett företag som var tidigt ute på en marknad håller sina kunder lojala i samband med att konkurrenssituationen förändras. Metod För att besvara syftet har en kvalitativ fallstudie om företaget MatHem gjorts, för att slutligen kunna dra en generaliserad slutsats. Där insamling av primärdata och sekundärdata har analyserats för att slutligen nå en slutsats. Slutsats Det undersökta företaget håller sina kunder lojala genom att ha en hög generell kvalitet. Vilket betyder att de har hög kvalitet på produkterna, väl fungerande kundservice, överträffar kundens förväntningar och ett brett sortiment. När konkurrenssituationen förändras har företaget inga speciella strategier för att hålla sina kunder lojala, eftersom att företaget inte ser de andra aktörerna som konkurrenter. Företaget är den dyraste aktören på marknaden, men differentierar sig med ekologiska produkter för att erhålla lojala kunder.

Faktorer på avdelningen som påverkar den kortvariga sjukfrånvaron : En fallstudie av tre avdelningar med olika storlek

Bakgrund: Sjukfrånvaron är ett fenomen som snabbt ökar i Sverige idag. Detta är något som kostar stora summor pengar varje år men trots detta finns relativt lite forskning på området. Den forskning som finns i området undersöker till stor del endast den långvariga sjukfrånvaron. Författarna av denna studie har tydligt identifierat en lucka i forskningen vad gäller kortvarig sjukfrånvaro. Syfte: Denna studie syftar därmed att undersöka storleken på avdelningen samt chefens kommunikation och interaktions påverkan på kortvarig sjukfrånvaro. Resultat: Undersökningen resultat är sammanställt ur dels en enkät som de anställda på tre avdelningar inom ett internationellt produktionsföretag fått besvara och dels tre intervjuer genomförda med en HR-chef och två chefer över avdelningarna. Resultatet blev att fem kategorikoder identifierades; Avdelningens storlek, Chefens kommunikation och interaktion, Frånvarokultur, Arbetsuppgifter och Hälsoarbete. Slutsats: Den främsta slutsats som denna undersökning resulterat i är att storleken på avdelningen påverkar de anställdas möjlighet snarare än deras tendens till att vara kortvarigt sjukfrånvarande. Den faktor som istället anses påverka den kortvariga sjukfrånvaron är hur chefen kommunicerar och integrerar med de anställda. Fokus bör därmed läggas vid denna faktor i försök att antingen minska eller kontrollera den kortvariga sjukfrånvaron på avdelningen

"Vad som behövs? Det är sällan glasklart!" : En studie kring en organisations tillväxt och växtvärksproblematik

I en organisation belägen på Dalarnas landsbygd framkommer det i en medarbetarundersökning att ett ökande missnöje finns hos de anställda, där flera av problemen kan kopplas till den kraftiga expansion som organisationen just nu genomgår. Även en positiv organisationsförändring som tillväxt kan alltså bidra till problem hos de anställda. Denna studie har avsett att undersöka vilka utmaningar och möjligheter som upplevs hos de anställda i organisationen kopplat till den tillväxtfas de genomgår. Detta genom åtta djupintervjuer där urvalet var såväl chefer, medarbetare som HR-ansvariga. Utifrån respondenternas upplevelse av situationen fann vi fyra stora problemområden; avsaknad av gemensamma rutiner, otydliga roller, bristfällig information och kommunikation samt brist på proaktivt arbete för att säkerställa medarbetarnas kompetens. Vårt empiriska material tyder på att organisationen har ett gap när det kommer till utvecklingen av såväl de mänskliga resurserna, arbetssystem som ledarskapet. Antalet anställda ökar i en högre takt än organisationens infrastrukturella processer, något som kan ses som en organisatorisk växtvärk. Med utgångspunkt från resultatet ger vi förslag på vilka aktiviteter HR-funktionen bör fokusera på. För att bemöta utvecklingsgapet samt förhindra att fler växtvärkssymptom uppstår anser vi att HR bör fokusera på ett proaktivt arbete. En nyckelfaktor som vi genom vår utvecklade modell visar är att ledaren är av stor vikt för hur organisationen och dess medarbetare hanterar en växtvärkssituation. HR bör därför ha en klar bild över vilket stöd verksamhetens ledare behöver för att kunna skapa värde för organisationen, ledarna och medarbetarna. Några generella förslag på HR-aktiviteter går däremot inte att ge eftersom, precis som tidigare forskning visar, verksamheters individuella situation och kontext avgör vilka aktiviteter som är aktuella.