Observations sur les termes culinaires dans deux San-Antonio de Frédéric Dard

Pro gradu-työni aihe on ruokaterminologiaa käsittelevät ranskan puhekielen ja Pariisin slangin lainasanat sekä kirjailija Frédéric Dardin alias San-Antonion (1921-2000) luomat, ruokatermistöön kuuluvat uudissanat ja -sanonnat kahdessa San-Antonio-romaanissa C'est mort et ça ne sait pas sekä Le fil à couper le beurre. Näissä ns. kioskikirjallisuutta edustavissa rikosromaaneissa seikkailee puheenparttaan ruoka-alan termeillä höystävä, "erikoistehtäviä" hoitava komisario ja naistenmies, San-Antonio. Ranskankielisessä arjen kielenkäytössä vilisee ruokaan liittyviä sanoja ja sanontoja muissakin kuin varsinaisissa ruuanvalmistus- ja ateriointiyhteyksissä. Halusin tarkastella, millaisena tämä yleisesti havaitsemani ilmiö todentuu Frédéric Dardin kahdessa romaanissa, jotka olen valinnut aineistokseni. Frédéric Dard käyttää romaaneissaan varsin omaperäistä kieltä: sekä puhekieltä että Pariisin slangia. Korpukseni koostuu romaaneista poimimistani ruoka-alan termistöä sisältävistä esimerkeistä, joita valmiiseen työhön tuli 228 kappaletta. Jaoin kaikki korpuksesta löytämäni ruokatermit kahteen luokkaan sen mukaan, oliko kirjailija lainannut käyttämänsä sanan tai ilmauksen puhekielestä tai Pariisin slangista (lainatermit), vai oliko hän luonut termin tai ilmauksen itse (neologismit). Määrittelin termin tai ilmauksen neologismiksi, jos se ei esiintynyt joko laisinkaan tai ainakaan kirjailijan tarkoittamassa merkityksessä seuraavissa sanakirjoissa: Le Dictionnaire du français argotique, populaire et familier; Le Dictionnaire de l'argot moderne; Le Dictionnaire du français non conventionnel; Le Dictionnaire de l'argot; Le Dictionnaire du français argotique et populaire; L'argot chez les vrais de vrai ja Trésor de la langue française. Varsinainen tutkimus perustuu sanojen ja ilmausten merkitysten selvittämiseen ja analysointiin. Lainatermien analyysillä tarkoitan lainatermien merkitysten selvitystä em. sanakirjojen avulla. Neologismit analysoin tarkemmin käyttäen em. sanakirjoja sekä tukeutuen gastronomisten ja erityisesti kielitieteellisten lähdeteosteni tarjoamiin rakenteellisiin ja semanttisiin muodostustapoihin ja tekemällä niistä tarvittavat yhteenvedot oikean merkityksen selvittämiseksi. Käsittelin aineiston kaikki ruokatermit. Niiden valtavan lukumäärän vuoksi analysoitavien esimerkkien määrää piti rajoittaa niin, että valmiiseen työhön jäi jokaisesta termistä enintään kaksi esimerkkiä kummastakin korpuksen kirjasta eli yhteensä 228 esimerkkiä. Muut esimerkit luetteloin työn lopusta löytyvään liitteeseen. Neologismianalyysissä selvisi, että Frédéric Dard suosi erityisesti semanttisia muodostustapoja eli olemassa olevan merkityksen muuttamista metaforien ja kielikuvien avulla. Dardin rikas terminologia ja hänen humoristiset oivalluksensa ovat osaltaan rikastuttaneet ranskan puhekieltä.Työssäni totean, että Pariisin slangia ja puhekieltä on totuttu pitämään sosiaalisesti sopimattomana, marginaalisten ryhmien kielenä, vaikka sen ilmauksia saattaa nykyisin kuulla jopa akateemikkojen käyttävän, ja ilmauksia on siirtynyt slangi- ja puhekielestä yleiskieleen. Toivon työni edistävän kiinnostusta kielitaidon parantamiseen San-Antonion tyyliin tutustumisen avulla sekä herättävän mielenkiintoa ranskan kielen vivahteikkuuteen ja monimuotoisuuteen muullakin kuin yleiskielen tasolla. Kielessä ei mielestäni voi olla sellaisia osa-alueita, joiden opiskelu ja osaaminen olisi tarpeetonta.

High-quality polar UV measurements : scientific analyses and transfer of the irradiance scale

The Earth's ecosystems are protected from the dangerous part of the solar ultraviolet (UV) radiation by stratospheric ozone, which absorbs most of the harmful UV wavelengths. Severe depletion of stratospheric ozone has been observed in the Antarctic region, and to a lesser extent in the Arctic and midlatitudes. Concern about the effects of increasing UV radiation on human beings and the natural environment has led to ground based monitoring of UV radiation. In order to achieve high-quality UV time series for scientific analyses, proper quality control (QC) and quality assurance (QA) procedures have to be followed. In this work, practices of QC and QA are developed for Brewer spectroradiometers and NILU-UV multifilter radiometers, which measure in the Arctic and Antarctic regions, respectively. These practices are applicable to other UV instruments as well. The spectral features and the effect of different factors affecting UV radiation were studied for the spectral UV time series at Sodankylä. The QA of the Finnish Meteorological Institute's (FMI) two Brewer spectroradiometers included daily maintenance, laboratory characterizations, the calculation of long-term spectral responsivity, data processing and quality assessment. New methods for the cosine correction, the temperature correction and the calculation of long-term changes of spectral responsivity were developed. Reconstructed UV irradiances were used as a QA tool for spectroradiometer data. The actual cosine correction factor was found to vary between 1.08-1.12 and 1.08-1.13. The temperature characterization showed a linear temperature dependence between the instrument's internal temperature and the photon counts per cycle. Both Brewers have participated in international spectroradiometer comparisons and have shown good stability. The differences between the Brewers and the portable reference spectroradiometer QASUME have been within 5% during 2002-2010. The features of the spectral UV radiation time series at Sodankylä were analysed for the time period 1990-2001. No statistically significant long-term changes in UV irradiances were found, and the results were strongly dependent on the time period studied. Ozone was the dominant factor affecting UV radiation during the springtime, whereas clouds played a more important role during the summertime. During this work, the Antarctic NILU-UV multifilter radiometer network was established by the Instituto Nacional de Meteorogía (INM) as a joint Spanish-Argentinian-Finnish cooperation project. As part of this work, the QC/QA practices of the network were developed. They included training of the operators, daily maintenance, regular lamp tests and solar comparisons with the travelling reference instrument. Drifts of up to 35% in the sensitivity of the channels of the NILU-UV multifilter radiometers were found during the first four years of operation. This work emphasized the importance of proper QC/QA, including regular lamp tests, for the multifilter radiometers also. The effect of the drifts were corrected by a method scaling the site NILU-UV channels to those of the travelling reference NILU-UV. After correction, the mean ratios of erythemally-weighted UV dose rates measured during solar comparisons between the reference NILU-UV and the site NILU-UVs were 1.007±0.011 and 1.012±0.012 for Ushuaia and Marambio, respectively, when the solar zenith angle varied up to 80°. Solar comparisons between the NILU-UVs and spectroradiometers showed a ±5% difference near local noon time, which can be seen as proof of successful QC/QA procedures and transfer of irradiance scales. This work also showed that UV measurements made in the Arctic and Antarctic can be comparable with each other.

Observations of production and transport of NOx formed by energetic particle precipitation in the polar night atmosphere

This work is focused on the effects of energetic particle precipitation of solar or magnetospheric origin on the polar middle atmosphere. The energetic charged particles have access to the atmosphere in the polar areas, where they are guided by the Earth's magnetic field. The particles penetrate down to 20-100 km altitudes (stratosphere and mesosphere) ionising the ambient air. This ionisation leads to production of odd nitrogen (NOx) and odd hydrogen species, which take part in catalytic ozone destruction. NOx has a very long chemical lifetime during polar night conditions. Therefore NOx produced at high altitudes during polar night can be transported to lower stratospheric altitudes. Particular emphasis in this work is in the use of both space and ground based observations: ozone and NO2 measurements from the GOMOS instrument on board the European Space Agency's Envisat-satellite are used together with subionospheric VLF radio wave observations from ground stations. Combining the two observation techniques enabled detection of NOx enhancements throughout the middle atmosphere, including tracking the descent of NOx enhancements of high altitude origin down to the stratosphere. GOMOS observations of the large Solar Proton Events of October-November 2003 showed the progression of the SPE initiated NOx enhancements through the polar winter. In the upper stratosphere, nighttime NO2 increased by an order of magnitude, and the effect was observed to last for several weeks after the SPEs. Ozone decreases up to 60 % from the pre-SPE values were observed in the upper stratosphere nearly a month after the events. Over several weeks the GOMOS observations showed the gradual descent of the NOx enhancements to lower altitudes. Measurements from years 2002-2006 were used to study polar winter NOx increases and their connection to energetic particle precipitation. NOx enhancements were found to occur in a good correlation with both increased high-energy particle precipitation and increased geomagnetic activity. The average wintertime polar NOx was found to have a nearly linear relationship with the average wintertime geomagnetic activity. The results from this thesis work show how important energetic particle precipitation from outside the atmosphere is as a source of NOx in the middle atmosphere, and thus its importance to the chemical balance of the atmosphere.

Dynamical processes in the stratosphere and upper troposphere and their influence on the distribution of trace gases in the polar atmosphere

Transport plays an important role in the distribution of long-lived gases such as ozone and water vapour in the atmosphere. Understanding of observed variability in these gases as well as prediction of the future changes depends therefore on our knowledge of the relevant atmospheric dynamics. This dissertation studies certain dynamical processes in the stratosphere and upper troposphere which influence the distribution of ozone and water vapour in the atmosphere. The planetary waves that originate in the troposphere drive the stratospheric circulation. They influence both the meridional transport of substances as well as parameters of the polar vortices. In turn, temperatures inside the polar vortices influence abundance of the Polar Stratospheric Clouds (PSC) and therefore the chemical ozone destruction. Wave forcing of the stratospheric circulation is not uniform during winter. The November-December averaged stratospheric eddy heat flux shows a significant anticorrelation with the January-February averaged eddy heat flux in the midlatitude stratosphere and troposphere. These intraseasonal variations are attributable to the internal stratospheric vacillations. In the period 1979-2002, the wave forcing exhibited a negative trend which was confined to the second half of winter only. In the period 1958-2002, area, strength and longevity of the Arctic polar vortices do not exhibit significant long-term changes while the area with temperatures lower than the threshold temperature for PSC formation shows statistically significant increase. However, the Arctic vortex parameters show significant decadal changes which are mirrored in the ozone variability. Monthly ozone tendencies in the Northern Hemisphere show significant correlations (|r|=0.7) with proxies of the stratospheric circulation. In the Antarctic, the springtime vortex in the lower stratosphere shows statistically significant trends in temperature, longevity and strength (but not in area) in the period 1979-2001. Analysis of the ozone and water vapour vertical distributions in the Arctic UTLS shows that layering below and above the tropopause is often associated with poleward Rossby wave-breaking. These observations together with calculations of cross-tropopause fluxes emphasize the importance of poleward Rossby wave breaking for the stratosphere-troposphere exchange in the Arctic.