A Curious Harpour in Helle : An Edition of the Commentary on the Orpheus Metre of De consolatione philosophiae in MS Thott 304,2

Tutkielmani on tekstieditio keskiaikaisesta kommentaarista, joka löytyy Kööpenhaminan Kuninkaallisen kirjaston käsikirjoituksesta Thott 304,2. Käsikirjoitus voidaan ajoittaa 1400-luvun ensimmäiselle neljännekselle ja se on kirjoitettu keskienglanniksi. Se sisältää John Waltonin runomuotoisen käännöksen Boethiuksen 500-luvun alussa latinaksi kirjoittamasta teoksesta De consolatione philosophiae (Filosofian lohdutus) sekä teosta kommentoivan proosamuotoisen kommentaarin. Käsikirjoitus on vaillinainen, mutta sen säilyneet foliot ovat enimmäkseen erittäin hyväkuntoisia. Itse käsikirjoitusta on tutkittu vain muutamissa artikkeleissa ja yhdessä tutkielmassa; kommentaarista ei ole toistaiseksi tehty kattavaa tutkimusta. Tavoitteeni onkin tuoda kommentaari keskiaikaisen filosofian, keskienglannin ja käsikirjoitusten tutkijoiden käytettäviin. Käsikirjoitus Thott 304,2 on esimerkki epätyypillisestä myöhäiskeskiaikaisesta maallikkomesenaattiudesta Englannissa. Tavanmukaisesti maallikkomesenaatit tukivat uskonnollisten tekstien tuottamista ja kääntämistä, kun taas Thott 304,2 sisältää käännöksen filosofisesta tekstistä. Sen lisäksi mesenaatti oli nainen, aatelistoon kuuluva Elizabeth Berkeley. Varsin harvinaiseksi käsikirjoituksen tekee sen painaminen kirjaksi 1500-luvun alussa. Kirjanpainajan käsikirjoituksen sivuille tekemistä merkinnöistä saadaan korvaamatonta tietoa varhaisesta painotekniikasta, sillä kirjanpainajien käyttämiä käsikirjoituskopioita ei ole säilynyt kovin runsaasti. Waltonin käännös on säilynyt yli kahdessakymmenessä käsikirjoituskopiossa, joista vain Thott 304,2 sisältää laajan kommentaarin. 1500-luvun painoksesta on jäljellä kolme kopiota, ja ne sisältävät saman kommentaarin kuin Thott 304,2. Valitsin editoitavaksi niin kutsuttua Orfeus-runoa kommentoivan osan kommentaarista, sillä se muodostaa ehjän kokonaisuuden ja sopii pituutensa puolesta Pro gradu -tutkielmaan. Orfeus-runo on myös yksi käsikirjoituksen kattavimmin kommentoiduista runoista. Editio on niin sanottu diplomaattinen transkriptio, jossa käsikirjoituksen piirteet on pyritty säilyttämään mahdollisimman tarkasti edition luettavuuden siitä kuitenkaan kärsimättä. Perinteisistä editioista poiketen tutkielmani sisältää myös kommentaarin ja Orfeus-runon transkriptiot, joissa rivijako, lyhenteet ja erikoismerkit on säilytetty. Näiden transkriptioiden toivon auttavan erityisesti käsikirjoituksessa esiintyvien lyhenteiden, erikoismerkkien ja kirjanpainajan merkintöjen tulkinnassa ja tutkimisessa. Editiota ja transkriptioita täydentävät nykyenglanniksi kirjoitettu lyhennelmä kommentaarista ja kuvat käsikirjoituksen sivuista, joilla editoimani kommentaari on. Tutkielmaan sisältyy alkuperäisen tekstin, käännöksen, kommentaarin ja käsikirjoituksen taustaa valottava osuus. Esittelen myös kaikki löytämäni lähteet, joissa käsikirjoitus on mainittu tai joissa sitä on tutkittu. Liitteeksi olen laatinut sanaston helpottamaan kommentaarin tulkitsemista.

Studies of Earth Dynamics with the Superconducting Gravimeter

The superconducting (or cryogenic) gravimeter (SG) is based on the levitation of a super­conducting sphere in a stable magnetic field created by current in superconducting coils. Depending on frequency, it is capable of detecting gravity variations as small as 10-11ms-2. For a single event, the detection threshold is higher, conservatively about 10-9 ms-2. Due to its high sensitivity and low drift rate, the SG is eminently suitable for the study of geodynamical phenomena through their gravity signatures. I present investigations of Earth dynamics with the superconducting gravimeter GWR T020 at Metsähovi from 1994 to 2005. The history and key technical details of the installation are given. The data processing methods and the development of the local tidal model at Metsähovi are presented. The T020 is a part of the worldwide GGP (Global Geodynamics Project) network, which consist of 20 working station. The data of the T020 and of other participating SGs are available to the scientific community. The SG T020 have used as a long-period seismometer to study microseismicity and the Earth s free oscillation. The annual variation, spectral distribution, amplitude and the sources of microseism at Metsähovi were presented. Free oscillations excited by three large earthquakes were analyzed: the spectra, attenuation and rotational splitting of the modes. The lowest modes of all different oscillation types are studied, i.e. the radial mode 0S0, the "football mode" 0S2, and the toroidal mode 0T2. The very low level (0.01 nms-1) incessant excitation of the Earth s free oscillation was detected with the T020. The recovery of global and regional variations in gravity with the SG requires the modelling of local gravity effects. The most important of them is hydrology. The variation in the groundwater level at Metsähovi as measured in a borehole in the fractured bedrock correlates significantly (0.79) with gravity. The influence of local precipitation, soil moisture and snow cover are detectable in the gravity record. The gravity effect of the variation in atmospheric mass and that of the non-tidal loading by the Baltic Sea were investigated together, as sea level and air pressure are correlated. Using Green s functions it was calculated that a 1 metre uniform layer of water in the Baltic Sea increases the gravity at Metsähovi by 31 nms-2 and the vertical deformation is -11 mm. The regression coefficient for sea level is 27 nms-2m-1, which is 87% of the uniform model. These studies are associated with temporal height variations using the GPS data of Metsähovi permanent station. Results of long time series at Metsähovi demonstrated high quality of data and correctly carried out offsets and drift corrections. The superconducting gravimeter T020 has been proved to be an eminent and versatile tool in studies of the Earth dynamics.

Grönlannin mannerjäätikön tulevaisuus: merenpinnan nousu maailmanlaajuisesti ja Itämerellä

Sea level rise is among the most worrying consequences of climate change, and the biggest uncertainty of sea level predictions lies in the future behaviour of the ice sheets of Greenland and Antarctica. In this work, a literature review is made concerning the future of the Greenland ice sheet and the effect of its melting on Baltic Sea level. The relation between sea level and ice sheets is also considered more generally from a theoretical and historical point of view. Lately, surprisingly rapid changes in the amount of ice discharging into the sea have been observed along the coastal areas of the ice sheets, and the mass deficit of Greenland and West Antarctic ice sheets which are considered vulnerable to warming has been increasing from the 1990s. The changes are probably related to atmospheric or oceanic temperature variations which affect the flow speed of ice either via meltwater penetrating to the bottom of the ice sheet or via changes in the flow resistance generated by the floating parts of an ice stream. These phenomena are assumed to increase the mass deficit of the ice sheets in the warming climate; however, there is no comprehensive theory to explain and model them. Thus, it is not yet possible to make reliable predictions of the ice sheet contribution to sea level rise. On the grounds of the historical evidence it appears that sea level can rise rather rapidly, 1 2 metres per century, even during warm climate periods. Sea level rise projections of similar magnitude have been made with so-called semiempirical methods that are based on modelling the link between sea level and global mean temperature. Such a rapid rise would require considerable acceleration of the ice sheet flow. Stronger rise appears rather unlikely, among other things because the mountainous coastline restricts ice discharge from Greenland. The upper limit of sea level rise from Greenland alone has been estimated at half a metre by the end of this century. Due to changes in the Earth s gravity field, the sea level rise caused by melting ice is not spatially uniform. Near the melting ice sheet the sea level rise is considerably smaller than the global average, whereas farther away it is slightly greater than the average. Because of this phenomenon, the effect of the Greenland ice sheet on Baltic Sea level will probably be rather small during this century, 15 cm at most. Melting of the Antarctic ice sheet is clearly more dangerous for the Baltic Sea, but also very uncertain. It is likely that the sea level predictions will become more accurate in the near future as the ice sheet models develop.

On Musical Self-Similarity : Intersemiosis as Synecdoche and Analogy

Self-similarity, a concept taken from mathematics, is gradually becoming a keyword in musicology. Although a polysemic term, self-similarity often refers to the multi-scalar feature repetition in a set of relationships, and it is commonly valued as an indication for musical coherence and consistency . This investigation provides a theory of musical meaning formation in the context of intersemiosis, that is, the translation of meaning from one cognitive domain to another cognitive domain (e.g. from mathematics to music, or to speech or graphic forms). From this perspective, the degree of coherence of a musical system relies on a synecdochic intersemiosis: a system of related signs within other comparable and correlated systems. This research analyzes the modalities of such correlations, exploring their general and particular traits, and their operational bounds. Looking forward in this direction, the notion of analogy is used as a rich concept through its two definitions quoted by the Classical literature: proportion and paradigm, enormously valuable in establishing measurement, likeness and affinity criteria. Using quantitative qualitative methods, evidence is presented to justify a parallel study of different modalities of musical self-similarity. For this purpose, original arguments by Benoît B. Mandelbrot are revised, alongside a systematic critique of the literature on the subject. Furthermore, connecting Charles S. Peirce s synechism with Mandelbrot s fractality is one of the main developments of the present study. This study provides elements for explaining Bolognesi s (1983) conjecture, that states that the most primitive, intuitive and basic musical device is self-reference, extending its functions and operations to self-similar surfaces. In this sense, this research suggests that, with various modalities of self-similarity, synecdochic intersemiosis acts as system of systems in coordination with greater or lesser development of structural consistency, and with a greater or lesser contextual dependence.

Helsingin lämpösaareke ajallisena ja paikallisena ilmiönä

The urban heat island phenomenon is the most well-known all-year-round urban climate phenomenon. It occurs in summer during the daytime due to the short-wave radiation from the sun and in wintertime, through anthropogenic heat production. In summertime, the properties of the fabric of city buildings determine how much energy is stored, conducted and transmitted through the material. During night-time, when there is no incoming short-wave radiation, all fabrics of the city release the energy in form of heat back to the urban atmosphere. In wintertime anthropogenic heating of buildings and traffic deliver energy into the urban atmosphere. The initial focus of Helsinki urban heat island was on the description of the intensity of the urban heat island (Fogelberg 1973, Alestalo 1975). In this project our goal was to carry out as many measurements as possible over a large area of Helsinki to give a long term estimate of the Helsinki urban heat island. Helsinki is a city with 550 000 inhabitants and located on the north shore of Finnish Bay of the Baltic Sea. Initially, comparison studies against long-term weather station records showed that our regular, but weekly, sampling of observations adequately describe the Helsinki urban heat island. The project covered an entire seasonal cycle over the 12 months from July 2009 to June 2010. The measurements were conducted using a moving platform following microclimatological traditions. Tuesday was selected as the measuring day because it was the only weekday during the one year time span without any public holidays. Once a week, two set of measurements, in total 104, were conducted in the heterogeneous temperature conditions of Helsinki city centre. In the more homogeneous suburban areas, one set of measurements was taken every second week, to give a total of 52.The first set of measurements took place before noon, and the second 12 hours, just prior to midnight. Helsinki Kaisaniemi weather station was chosen as the reference station. This weather station is located in a large park in the city centre of Helsinki. Along the measurement route, 336 fixed points were established, and the monthly air temperature differences to Kaisaniemi were calculated to produce monthly and annual maps. The monthly air temperature differences were interpolated 21.1 km by 18.1 km horizontal grid with 100 metre resolution residual kriging method. The following independent variables for the kriging interpolation method were used: topographical height, portion of sea area, portion of trees, fraction of built-up and not built-up area, volumes of buildings, and population density. The annual mean air temperature difference gives the best representation of the Helsinki urban heat island effect- Due to natural variability of weather conditions during the measurement campaign care must be taken when interpretation the results for the monthly values. The main results of this urban heat island research project are: a) The city centre of Helsinki is warmer than its surroundings, both on a monthly main basis, and for the annual mean, however, there are only a few grid points, 46 out of 38 191, which display a temperature difference of more than 1K. b) If the monthly spatial variation is air temperature differences is small, then usually the temperature difference between the city and the surroundings is also small. c) Isolated large buildings and suburban centres create their own individual heat island. d) The topographical influence on air temperature can generally be neglected for the monthly mean, but can be strong under certain weather conditions.