Visualization of geochemical data on maps at the Geological Survey of Finland

Software for presentation of geochemical data on maps has been integrated into a user-friendly package, ALKEMIA, at the Geological Survey of Finland (GSF). ALKEMIA contains procedures for generating dot maps, colour surface maps, shaded relief maps, and vector images, and for interpolating and smoothing irregularly gridded data. Combining dots and colour surfaces provides a means of visually integrating up to three variables on a map, revealing the spatial relationships between them. The methods employed are described in detail, particularly the moving weighted median, which has been widely used at the GSF for interpolating and smoothing geochemical and other numerical data. Several geochemical and oncological atlases and series of maps have been produced with these methods.     

The amphibolite-granulite facies transition in West Uusimaa, S.W. Finland. A fluid inclusion study

This work presents the results of a fluid inclusion study of an amphibolite-granulite facies transition in West Uusimaa, S.W. Finland. Early fluid-inclusions in the granulite facies area are characteristically carbonic (CO₂), in contrast to predominantly aqueous early inclusions in the amphibolite facies area. These early inclusions can be related to peak metamorphic conditions (750-820°C and 3-5 kbar for peak granulite facies metamorphism). Relatively young CO₂ inclusions with low densities (<0.8g/cm³) indicate that the first part of the cooling history of the rocks was characterized by a near isothermal uplift.
N₂-CH₄ inclusions, with compositions ranging between pure CH₄ and pure N₂ (Raman spectral analysis), were found in the whole area. They are probably syn- or even pre-early inclusions. Only nearly critical homogenizing inclusions have been found (low density). Pressure estimates, based on densities of early fluid inclusions, show that the rapid transition of amphibolite towards granulite facies metamorphism is virtually isobaric. Granulite facies metamorphism in West Uusimaa is a thermal event, probably induced by the influx of hot, CO₂-bearing fluids.     

BUILDING A FACADE FOR FINLAND: HELSINKI IN TOURISM IMAGERY*

Tourist destination promoters compose visual images and arrange them in brochures in order to communicate a coherent and attractive story. In a changing socioeconomic and political context, the city officials of Helsinki recognized a need for systematic promotion in the 1950s. In this article I examine 127 images published in ten tourism brochures produced by the Excursion Section of the Sport and Excursion Office of Helsinki between 1954 and 1963. The data‐driven, content‐analytical study shows how the images served a political identity project aimed at creating a sense of national solidarity among the Finns and to show international audiences that Finland is a modern nation. As a means of gaining acceptance in the West, support of citizenship education included emphasis on national symbols and signs of well‐being and visualization of urban tourism.     

Estimating winter evaporation in boreal forests with operational snow course data

Snow course measurements from 11 sites located in eastern and northern Finland were used to estimate the total interception evaporation of a winter season for different forest categories. We categorized the sites based on forest density and tree species. Results showed that interception loss from gross precipitation increased with forest density and approached 30% for a forest with the highest density class. Interception loss for the most common forest density class was 11%. Interception losses were slightly larger in spruce forests than in pine, deciduous, or mixed forests. We provide suggestions as to how to design snow surveys to estimate wintertime interception evaporation better. Rough terrain and transition zones between forest and open areas should be avoided. Since evaporation fraction was strongly dependent on tree crown characteristics, snow course data should include direct estimates of canopy closure. Qualitative observations made by different observers should be given a reference frame to ensure comparability of records from different sites. Copyright © 2003 John Wiley & Sons, Ltd.     

THE ROLE OF ATMOSPHERIC CIRCULATION PATTERNS IN AGROCLIMATE VARIABILITY IN FINLAND, 1961–2011

This study evaluates interannual variations and trends in growing season daily temperature sum and daily precipitation sum in Finland during 1961–2011, and their connections to well known atmospheric circulation patterns. Changes in summer (June–August) climate partially explain changes in growing season daily temperature sum and daily precipitation sum over Finland, which naturally decreased from south to north. On a national scale, growing season warmed and became wetter during 1961–2011, as growing season daily temperature sum and daily precipitation sum significantly (p < 0.05) increased by 5.01 ± 3.17°C year^–1 and 1.39 ± 0.91 mm year^–1, respectively. The East Atlantic pattern was the most influential atmospheric circulation pattern for variations in growing season daily temperature sum (rho = 0.40) across Finland and the East Atlantic/West Russia pattern was most influential for growing season daily precipitation sum variability (rho = –0.54). There were significant (p < 0.05) increasing trends in growing season daily temperature sum and daily precipitation sum throughout Finland during 1961–2011. Increased growing season daily temperature sum was mainly observed in northern, central, western, eastern and coastal areas of south‐western Finland. This warming was positively associated with the East Atlantic pattern in the north, centre and south, but negatively associated with the East Atlantic/West Russia pattern in eastern Finland. Increased GSP mostly occurred in southern, eastern, western, central, northern and north‐western Finland. These wetting trends were positively correlated with the East Atlantic pattern in the north and negatively correlated with the Polar pattern in the south and the East Atlantic/West Russia pattern in the east, west, centre and north‐east of Finland. The overall agroclimatic year‐to‐year variability in Finland between 1961 and 2011 was mostly linked to variations in the East Atlantic and East Atlantic/West Russia patterns.     

Regional innovation systems,high-technology development,and governance in the periphery: The case of Northern Finland

The article examines high-technology development networks in peripheral areas using the case of Northern Finland (as defined by the EU under its Structural Funds programme). Few material and social resources and long distances between key development actors are challenging for research and the development of technologies targeted at global markets. The case study concerns the regional innovation system-based Multipolis network, which brings together technology-related actors in Northern Finland, located on both sides of the Arctic Circle, in an area of c.155,000 km² and with a population of 0.7 million. The results of the research, which used Q-methodology, reveal that networking is needed between technology development actors in the region and at various spatial levels. However, conflicting viewpoints on the development of Northern Finland exist, and indicate a mismatch between competitiveness policies to support high-technology development and regional policies to promote local employment. It is recommended that more attention should be paid to the governance of technology development in peripheral areas.     

Power and influence tactics in the promotion of regional development: An empirical analysis of the work of Finnish regional development officers

Increased complexity and rapid pace of change demand more from people responsible for regional development at various levels of activity. This paper has its roots in a belief that the more complex situations are, the more regional development is dependent on the leadership and network management capacity of key individuals. Studying more deeply the roles that various individuals, and the coalitions formed by them, have in institutionalisation, deinstitutionalisation and reinstitutionalisation processes might provide us with additional analytical leverage in regional development studies. This paper focuses on diffuse networks of dispersed powers from a Finnish regional development officer’s point of view. Regional development officers are those people whose job it is to boost the economic development of their respective regions in Finland.The research questions discussed here are: (a) What kind of power is exercised by Finnish regional development officers; and (b) how do regional development officers aim to gain influence for their efforts to promote regional development? The empirical research is based on data gathered (a) through 41 interviews with Finnish actors responsible for the promotion of economic development in city governments, technology centres, regional development agencies, and ministries and other national bodies, and (b) through internet survey of development officers at local, regional and national levels (531 respondents, response rate 51.8%). The survey was designed to solicit information about power and influence tactics in the context of regional development. The empirical analysis shows, for example, how interpretive power and network power are more important for regional development officers than institutional and resource power, and how indirect influence tactics surpass direct tactics.     

Estimation of weathering rates for critical load calculations in Finland

 The formation of base cations through mineral weathering in forest soils is one of the key parameters in calculating critical loads. Weathering rates in Finland have been estimated using a variety of methods. In the first approach, three weathering rate categories were assigned to soils according to the bedrock type. The second approach was based on an empirical relationship obtained from Swedish field studies. Changes in zirconium content through the soil profile were used to estimate element losses in soil after deglaciation. These calculated losses correlated well with the total calcium and magnesium concentrations in till C-horizons and the effective temperature sum (ETS). Comprehensive geochemical data for the parent till fine fraction (<0.06 mm) was available through the reconnaissance scale till geochemical mapping program of the Geological Survey of Finland (GSF). The equations obtained from Swedish studies were based on the use of the coarse (<2.0 mm) till fraction, and the differences in element concentrations between the fine and coarse size fractions remained a potential source of uncertainty estimating overall weathering rates. In the third approach, new geochemical data from the <2.0 mm till fraction from southern Finland were used to make new weathering rate estimates. The use of soil geochemistry instead of bedrock map classification clearly led to an improvement in the estimates of soil weathering rates in glacied terrains. The use of the fine till fraction (<0.06 mm) in the zirconium approach generally resulted in overestimations of the weathering rate. The new geochemical data for the coarse till fraction (<2 mm) are now consistent with the input requirements of the zirconium method, although the results still require further evaluation. Finnish soil profiles have a shorter weathering history than most of the Swedish ones and the uppermost layer in Finnish podsols has in some cases developed in a different till layer than the C-horizon. Received: 15 October 1995 · Accepted: 8 March 1996