Lapsi ulkomailta – vanhempien rooli adoptiolapsen identiteetin kehityksessä

The importance of open discussion with the adopted child and his parents about adoption and ethnicity is often emphasized in adoption literature (Kirk 1964; Grotevant 1999; Carli & Dalen 1999). The child should have the possibility of constructing a harmonious view of himself, which consists of his history before adoption, ethnicity and the social environment’s conception of him. The purpose of this study was to examine the Finnish adoptive parents’ supportive role in relation to their child’s adoptive and ethnic identity and the social environment’s disposition to the child as witnessed by the parents. The first research problem was to find out how the parents support their child’s adoptive identity formation. The second problem was to find out if the parents want to support the child’s ethnic identity. The third problem was regarding the environment’s disposition to the child and family. The hypothesis was that Finnish adoptive parents are well aware of the problems of adoption and they have been well selected, so they have the aspirations and skills to help their child with his identity formation. The focus of this study was on Finnish parents who had adopted internationally, from whom 58 answers were obtained. The data was collected with an Internet based questionnaire. The questions were mostly qualitative. The analysis was directed by the theory, so that the analysis units were obtained from the main questions of international adoption and identity formation. The results expressed that the adoptive parents want to support their child’s adoption identity. They accept their child’s questions regarding his history, and that they did not want to conceal any details about their child’s life, even if they felt that it was a sensitive issue for them. The main problem was that there was no information available on the child’s history. Contact with the biological parents was almost impossible because there was hardly any information on them. Instead the parents were in contact with the children’s home because they felt that it had an important role as the child’s former home. The parents felt that the child’s birth culture was of importance and they mainly offered aspects of it informally daily. Parents who stressed their child’s Finnish identity were concerned that their child would not form a feeling of being Finnish. However, the majority wished that their child would have a multicultural identity. The parents felt that the environment regarded the child positively and the possibility of upcoming problems was tackled by discussing them beforehand with the child and environment.

Optical Studies of the Antarctic Glacio-Oceanic System

The Antarctic system comprises of the continent itself, Antarctica, and the ocean surrounding it, the Southern Ocean. The system has an important part in the global climate due to its size, its high latitude location and the negative radiation balance of its large ice sheets. Antarctica has also been in focus for several decades due to increased ultraviolet (UV) levels caused by stratospheric ozone depletion, and the disintegration of its ice shelves. In this study, measurements were made during three Austral summers to study the optical properties of the Antarctic system and to produce radiation information for additional modeling studies. These are related to specific phenomena found in the system. During the summer of 1997-1998, measurements of beam absorption and beam attenuation coefficients, and downwelling and upwelling irradiance were made in the Southern Ocean along a S-N transect at 6°E. The attenuation of photosynthetically active radiation (PAR) was calculated and used together with hydrographic measurements to judge whether the phytoplankton in the investigated areas of the Southern Ocean are light limited. By using the Kirk formula the diffuse attenuation coefficient was linked to the absorption and scattering coefficients. The diffuse attenuation coefficients (Kpar) for PAR were found to vary between 0.03 and 0.09 1/m. Using the values for KPAR and the definition of the Sverdrup critical depth, the studied Southern Ocean plankton systems were found not to be light limited. Variabilities in the spectral and total albedo of snow were studied in the Queen Maud Land region of Antarctica during the summers of 1999-2000 and 2000-2001. The measurement areas were the vicinity of the South African Antarctic research station SANAE 4, and a traverse near the Finnish Antarctic research station Aboa. The midday mean total albedos for snow were between 0.83, for clear skies, and 0.86, for overcast skies, at Aboa and between 0.81 and 0.83 for SANAE 4. The mean spectral albedo levels at Aboa and SANAE 4 were very close to each other. The variations in the spectral albedos were due more to differences in ambient conditions than variations in snow properties. A Monte-Carlo model was developed to study the spectral albedo and to develop a novel nondestructive method to measure the diffuse attenuation coefficient of snow. The method was based on the decay of upwelling radiation moving horizontally away from a source of downwelling light. This was assumed to have a relation to the diffuse attenuation coefficient. In the model, the attenuation coefficient obtained from the upwelling irradiance was higher than that obtained using vertical profiles of downwelling irradiance. The model results were compared to field measurements made on dry snow in Finnish Lapland and they correlated reasonably well. Low-elevation (below 1000 m) blue-ice areas may experience substantial melt-freeze cycles due to absorbed solar radiation and the small heat conductivity in the ice. A two-dimensional (x-z) model has been developed to simulate the formation and water circulation in the subsurface ponds. The model results show that for a physically reasonable parameter set the formation of liquid water within the ice can be reproduced. The results however are sensitive to the chosen parameter values, and their exact values are not well known. Vertical convection and a weak overturning circulation is generated stratifying the fluid and transporting warmer water downward, thereby causing additional melting at the base of the pond. In a 50-year integration, a global warming scenario mimicked by a decadal scale increase of 3 degrees per 100 years in air temperature, leads to a general increase in subsurface water volume. The ice did not disintegrate due to the air temperature increase after the 50 year integration.

Expected Performance of the ATLAS Experiment - Detector, Trigger and Physics

A detailed study is presented of the expected performance of the ATLAS detector. The reconstruction of tracks, leptons, photons, missing energy and jets is investigated, together with the performance of b-tagging and the trigger. The physics potential for a variety of interesting physics processes, within the Standard Model and beyond, is examined. The study comprises a series of notes based on simulations of the detector and physics processes, with particular emphasis given to the data expected from the first years of operation of the LHC at CERN.