On the ability of statistical wind-wave models to capture the variability and long-term trends of the North Atlantic winter wave climate

A dynamical wind-wave climate simulation covering the North Atlantic Ocean and spanning the whole 21st century under the A1B scenario has been compared with a set of statistical projections using atmospheric variables or large scale climate indices as predictors. As a first step, the performance of all statistical models has been evaluated for the present-day climate; namely they have been compared with a dynamical wind-wave hindcast in terms of winter Significant Wave Height (SWH) trends and variance as well as with altimetry data. For the projections, it has been found that statistical models that use wind speed as independent variable predictor are able to capture a larger fraction of the winter SWH inter-annual variability (68% on average) and of the long term changes projected by the dynamical simulation. Conversely, regression models using climate indices, sea level pressure and/or pressure gradient as predictors, account for a smaller SWH variance (from 2.8% to 33%) and do not reproduce the dynamically projected long term trends over the North Atlantic. Investigating the wind-sea and swell components separately, we have found that the combination of two regression models, one for wind-sea waves and another one for the swell component, can improve significantly the wave field projections obtained from single regression models over the North Atlantic.

Caves as a Winter Refuge by a Neotropical Harvestman (Arachnida, Opiliones)

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

Problematiska ljudkvalitetsskillnader vid liveproduktioner i samma lokal : En studie av upplevd ljudkvalitet vid två DJ-akters framträdanden under Dreamhack Winter 2014

Syftet med denna undersökning är bidra med förklaringar till varför upplevda ljudkvalitetsskillnader kan uppstå mellan olika akters framträdanden vid event och festivaler trots att de använder samma utrustning och är i samma lokal och att förklaringarna ska utgöra en kunskapskälla för dem som eftersträvar en god ljudkvalité vid liveframträdanden. De metoder som har används är fallstudie, webbenkät, intervjuer och egen observation. Webbenkäten användes på Dreamhack Winter 2014 där en grupp undersökningsdeltagare svarade på frågor om två olika DJ-akter på scenen i D-hallen, Elmia. Fem personer deltog som intervjupersoner: scenansvarig från Dreamhack, tre ljudtekniker ifrån olika ställen i Sverige och en person som jobbar med ljudteknisk konsultation och ljudmätning. Samtliga intervjuer genomfördes via mail. Intervjuerna eftersträvade att ge kunskap om dessa personers funderingar kring ljudkvalitetsproblemet och scenansvarig svarade på frågor om scenen på Dreamhack. En observation av upplevd ljudkvalitet och ljudteknikernas arbetssätt genomfördes av mig själv på Dreamhack Winter 2014. Resultatet från såväl enkätundersökningen som den egna observationen visar att inga stora upplevda skillnader fanns mellan de två akterna på Dreamhack Winter 2014. De upplevda skillnader som observerades var negativa anmärkningar, så som mängden bas och ljudstyrka. Intervjuerna visade på flera gemensamma åsikter bland ljudteknikerna angående förklaringar till ljudkvalitetsskillnader vid event som Dreamhack Winter 2014 där de ansåg att en kunnig och erfaren ljudtekniker, duktiga musiker, väl genomförd soundcheck och bra och rätt användande av utrustningen på scen krävs för att uppnå en upplevd god ljudkvalitet live. De förklaringar som finns enligt mina analyser och bland ljudteknikerna till negativa ljudkvalitetsskillnader inom liveljud i samma lokal är att ljudteknikern och musikerna är olika duktiga. Utrustning, soundcheck och akustik påverkar också kvalitén. Undersökningens sammantagna resultat tyder på att de upplevda ljudkvalitetetsskillnader som fanns på Dreamhack Winter 2014 berodde på bristande kompetens och engagemang hos tjänstgörande ljudtekniker och upplevda skillnader i bas- ljudnivå i de två DJ-akternas mixar.

Gay and Lesbian Life at Colby 1969-1974

The history of a gay and lesbian student community at Colby seems to point to the difficulty of visibility. For students who were able to find others like themselves, their group of lesbian and gay friends had to remain underground. For students who were grappling with their newly found, socially stigmatized sexuality, the experience was isolating if they did not know where to find others like themselves. This paper seeks to address the social forces that kept sexually variant students from expressing their sexual identities openly on campus. Part of this difficulty is attributable to the compulsory heterosexuality assumed by general American society at the time, manifested in the silence or outright hostility directed against homosexuals. Naturally, Colby students replicated this assumption. Some of the students we interviewed seemed to internalize compulsory heterosexuality, while it was forced upon others. Religion and psychology were two methods of enforcing heterosexuality that were relevant to the people we interviewed. Another significant obstacle to visibility was Colby's location and the nature of Colby's student body. Waterville, unlike more urban cities, did not have a history of gay life, and thus an established gay community or gay identity into which one could be socialized. Colby, as a small, homogeneous and isolated space, posed difficulties in establishing a gay community as the population to draw from was small and regulated.

DEVELOPING A MODEL FOR PEDESTRIAN ROUTE SELECTION AT COLBY

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A SPATIAL ANALYSIS OF IMPERVIOUS SURFACES AT COLBY COLLEGE IN 1965 AND 2006

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SPATIAL ANALYSIS OF COLBY COLLEGE TRAILS: PERKINS ARBORETUM AND RUNNALS HILL

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SOLAR PANEL MODELING ON SUITABLE ROOFS AT COLBY

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ANALYSIS OF FUTURE CONSTRUCTION POSSIBILITIES ON THE COLBY COLLEGE CAMPUS

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Monitoring Surface Displacement of the Colby Green Retaining Pond Dams

The Colby Green is a campus expansion project which began in October of 2003. The construction would result in three new buildings, additional parking, and an elliptical 75,000-squarefoot green southeast of Mayflower Hill Drive. There were also plans for the construction of three run-off management and sediment ponds below the green, to manage flooding of the green. Three drains in the green transport water to the three retaining ponds which slowly disperse water into the surrounding environment. The ponds were created by constructing earthen dams around the drain outlets. The dams are composed of soil, cobbles, and boulders procured from the surrounding excavation site. Unfortunately, earthen dams are susceptible to many types of erosion which result in their failure. In this case the potential for clay and silt from the underlying Presumpscot Formation to mix with the soil in the earthen dams raised concerns with regards to frost action. In order to monitor the surface displacement of the dams I drove 92 poles into the ground in 8 straight lines across the faces of the dams in the fall of 2005. I returned to the sites during and after the spring thaw of 2006, to check for any signs of movement resulting from frost-heave, surface creep, or any other form of mass wasting. Fortunately, there was no recordable sign of movement in the stakes across any of the retaining ponds. The dams appear to be functioning as designed.

DETAILED MAP AND RECREATIONAL SUITABILITY ASSESSMENT OF THE COLBY TRAIL SYSTEM

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LIGHT COVERAGE ON COLBY COLLEGE CAMPUS

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WIND TURBINE VISIBILITY ON THE COLBY CAMPUS

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