This thesis analyses the impacts of winter snowpack and subsequent spring and summer liquid precipitation on low flows in the warm season. Meltwater is an important source of groundwater recharge. From groundwater storage streams are donated during summer months. Snow accumulation during cold season is reduced and snowmelt occurs earlier, which is a result of climate change and leads to lower groundwater recharge rates. That is the reason why change in snow cover dynamics affects summer low flows. Main goals of this thesis are to analyse how snow cover affects low flows I warm season and to compare it with impact of spring and summer precipitation. A conceptual runoff model HBV-light has been used to simulate the snow water equivalent (SWE) and streamflow from three mountain catchments. The integrated multi-variable model calibration procedure was used to calibrate the model. The model was used to simulate the snow and streamflow from 1981 to 2014. Besides the mentioned simulation, two hypothetical scenarios have been performed. These two scenarios accounted for reduced spring and summer liquid precipitation. In the first scenario, precipitation after maximum annual SWE was reduced to 75% of the real measured precipitation. In the second scenario, precipitation was reduced to 50% of the real...

The master´s thesis deals with snow cover monitoring especially in area Orlické mountains. For identification changes, which are related to variable loads on snow cover of temperature, humidity and gravity, has been selected indirect electrical method of measuring electrical impedance spectrometry. This method is described in the work and the results of monitoring are published in graphical form and are commented.

This thesis deals with snow cover mapping by using time-series of SAR images of the sensors ENVISAT ASAR and TerraSAR-X. The methodology is based on the so-called Nagler's algorithm, which is based on determination of the change of absorption of radar signal due to the liquid water content in the snow cover. The resulting ratio image is classified into the areas with wet snow or without it according to the selected threshold value. The results are compared with the maps of snow cover derived from MODIS optical data and with data from meteorological stations of CHMI. The main aims of this work are to suggest most suitable conditions (time of the year, weather) for acquisition of reference images, to find the change of the threshold value with respect the chosen reference image and the type of land cover. The same methodology should then be applied on the radar data of shorter wavelength. The obtained results will be further used for improving the methodology of snow cover mapping from SAR data in the Czech Republic.

Title: Snow water content modelling in small catchments This work deals with modeling of amount of snow cover, snow water equivalent, respectively, on an experimental catchment in the Jizerské hory Mts. Measuring and modelling of the snow cover is an important part of water management practice from the perspective of reservoir operation and flood management. The first part of this thesis describes physical-geographical characteristics of the Jizerské hory Mts.especially from the climatological and hydrological point of view but also other charakteristics and conditions that may affect the dynamic of snow accumulation and melting are described with detailed focus on the experimental catchment of Černá Desná river - Jezdecká. Two modelling approaches were applied to simulate snow water equivalent (SWE) based on observed precipitation and temperature. Beside the well knowen SNOW17 model a simple method based on heat index was developed in this work and its parameters were calibrated based on measured timeseries of daily average air temperature, daily precipitation and observed SWE for winter periods 2001 to 2009. Both methods provided reasonably accurate estimates of SWE over the tested period, however it was found that the results for winters with extreme conditions (very warm or very cold) are less...

The precipitation falling as rain or snow has different impact on regional water resources and their annual distribution. Shift from solid to liquid form of precipitation following the increase of the surface air temperatures could be important because such change could influence the timing of spring runoff and cause water scarcity in summer. In this study, the spatial and temporal variations of ratio of snowfall to total precipitation (Sf), mean air temperature, day of year of melt-out and winter and spring runoff is analysed. Data were examined for 11 meteorological and 6 hydrological stations in the mountains catchment in Czechia for November-April 1965-2014. Data were analyzed using the Mann-Kendall trend test. Major results show that Sf has been decreasing strongly throughout the whole examined area, with the strongest decrease in the foothill area of the northern mountains of Czechia. Stronger decrease is observed in lower elevations, at the stations with meant air temperature close to melt temperature. Strongest decrease was observed in March and the weakest decrease was observed in December and April, The significant decreases in Sf are associated with large increase in mean winter air temperatures. Due to the increasing mean air temperature in the cold season, the total rainfall is...

<p>Snö har en stor betydelse för oss inom hydrologin samt ekologin. Inom hydrologin har snön inverkan på våra vattendrag under vinter och vår dessutom har den en stor betydande roll för elektricitetsproduktionen via vattenkraft. För ekologin ger snön isolering för växter, marken och skydd för mindre djur arter. Snöförhållanden förklarar också ofta naturkatastrofer, så som lavinrisker och översvämningar i vattendragen. Ökad kunskap om snöegenskaper skulle kunna hjälpa oss att förstå alla ovan nämnda skeenden bättre.</p><p>På Abiskos naturvetenskapliga forskningsstation har det sedan år 1961 till nu gjorts snöprofilsmätningar, där snötäckets egenskaper, tjocklek, snölagrets täthet/hårdhet, snö kristallernas fasthet, snökornens storlek och snöns torrhet uppskattas. Dessa mätningar utgör grunden till denna studie där syftet är att klimatologiskt undersöka den inre snöstrukturen.</p><p>Undersökningen av snöns inre struktur ger oss en tydlig bild av att kategorin is förekommer mycket ofta i snötäcket och att dess tjocklek är mycket tunn. Under de senaste 15-åren (1993-2007) har kategorin is utgjorts till 25% av alla egenskaper i snötäckets översta lager. Vi kan även se att snön har blivit mycket blötare under våren för perioden 1993-2007 (senaste 15 åren) speciellt under maj månad. Att detta är klara och distinkta spår på den ökade lufttemperaturen är det inga tvivel på. Tydliga spår av metamorfosen i snötäcket ses när kategorin mycket lucker och lucker har ökat kraftigt i det understa lagret de senaste åren, något som även förklarar ökade lavinrisker i området.</p><p>Snödjupet har minskat under de senaste 15 åren (1993-2007) under hösten (oktober och november) i jämförelse med de andra två 15-års perioderna (1961-1992), men snölagrets tjocklek har däremot ökat under våren.</p> / <p>Snow is of great importance to our environment in ways such as hydrological and ecological. When speaking in terms of hydrology, snow affects our water streams and has a great influence on hydropower. In ecological purposes, snow is a good isolator for vegetation, soil and it also gives shelter for smaller animals. Snow conditions often explain natural disaster, such as risks for avalanches and submergence in the streams. Understanding the fundamentals of snow properties would give scientist a greater understanding of snow and its effects on our environment.</p><p>Snow profile measurements have been made in Abisko research centre since 1961 until present time. Measurements have been done on snow cover properties, such as the thickness of the snow layer, grain size, snow layer hardness, grain compactness and the dryness of the snow. Collected data from Abisko research centre is the foundation of this study where our objective is to analyze the inner snow structure. This will give us a greater understanding of how snow has been behaving historically.</p><p>Result of this study illustrates that category ice occurs very frequent in the snow cover and its thickness is very thin. During the last 15-years (1993-2007) has the category ice constitute up to 25% of all the properties in the snow cover in the upper layer. We can also see that the snow cover has drastically become more wet during spring specially for the month may and there is no doubt that the increased air temperature is behind it. There are also distinct signs of metamorphoses in the snow cover which can explain the increased risks for avalanches in the area.</p><p>Results also shows that the snow depth has decreased during the last 15 years (1993-2007) in autumn (October and November) in comparison with the other 15-year periods (1961-1992), but on the other hand the snow layer thickness has increased during the spring.</p>

Snö har en stor betydelse för oss inom hydrologin samt ekologin. Inom hydrologin har snön inverkan på våra vattendrag under vinter och vår dessutom har den en stor betydande roll för elektricitetsproduktionen via vattenkraft. För ekologin ger snön isolering för växter, marken och skydd för mindre djur arter. Snöförhållanden förklarar också ofta naturkatastrofer, så som lavinrisker och översvämningar i vattendragen. Ökad kunskap om snöegenskaper skulle kunna hjälpa oss att förstå alla ovan nämnda skeenden bättre. På Abiskos naturvetenskapliga forskningsstation har det sedan år 1961 till nu gjorts snöprofilsmätningar, där snötäckets egenskaper, tjocklek, snölagrets täthet/hårdhet, snö kristallernas fasthet, snökornens storlek och snöns torrhet uppskattas. Dessa mätningar utgör grunden till denna studie där syftet är att klimatologiskt undersöka den inre snöstrukturen. Undersökningen av snöns inre struktur ger oss en tydlig bild av att kategorin is förekommer mycket ofta i snötäcket och att dess tjocklek är mycket tunn. Under de senaste 15-åren (1993-2007) har kategorin is utgjorts till 25% av alla egenskaper i snötäckets översta lager. Vi kan även se att snön har blivit mycket blötare under våren för perioden 1993-2007 (senaste 15 åren) speciellt under maj månad. Att detta är klara och distinkta spår på den ökade lufttemperaturen är det inga tvivel på. Tydliga spår av metamorfosen i snötäcket ses när kategorin mycket lucker och lucker har ökat kraftigt i det understa lagret de senaste åren, något som även förklarar ökade lavinrisker i området. Snödjupet har minskat under de senaste 15 åren (1993-2007) under hösten (oktober och november) i jämförelse med de andra två 15-års perioderna (1961-1992), men snölagrets tjocklek har däremot ökat under våren. / Snow is of great importance to our environment in ways such as hydrological and ecological. When speaking in terms of hydrology, snow affects our water streams and has a great influence on hydropower. In ecological purposes, snow is a good isolator for vegetation, soil and it also gives shelter for smaller animals. Snow conditions often explain natural disaster, such as risks for avalanches and submergence in the streams. Understanding the fundamentals of snow properties would give scientist a greater understanding of snow and its effects on our environment. Snow profile measurements have been made in Abisko research centre since 1961 until present time. Measurements have been done on snow cover properties, such as the thickness of the snow layer, grain size, snow layer hardness, grain compactness and the dryness of the snow. Collected data from Abisko research centre is the foundation of this study where our objective is to analyze the inner snow structure. This will give us a greater understanding of how snow has been behaving historically. Result of this study illustrates that category ice occurs very frequent in the snow cover and its thickness is very thin. During the last 15-years (1993-2007) has the category ice constitute up to 25% of all the properties in the snow cover in the upper layer. We can also see that the snow cover has drastically become more wet during spring specially for the month may and there is no doubt that the increased air temperature is behind it. There are also distinct signs of metamorphoses in the snow cover which can explain the increased risks for avalanches in the area. Results also shows that the snow depth has decreased during the last 15 years (1993-2007) in autumn (October and November) in comparison with the other 15-year periods (1961-1992), but on the other hand the snow layer thickness has increased during the spring.

The Mountain Hemlock (MH) zone includes all subalpine forests along British Columbia’s coast. It occurs at elevations where most precipitation falls as snow and the growing season is less than 4 months long. The zone includes the continuous forest of the forested subzones and the tree islands of the parkland subzones (Figure 1). Old-growth stands are populated by mountain hemlock, Pacific silver fir, and Alaska yellow-cedar, and are among the least-disturbed ecosystems in the world. Canopy trees grow slowly and are commonly older than 600 years, while some Alaska yellow-cedars may be up to 2000 years old. Early regeneration failures followed slashburning and the planting of unsuitable species. Currently, the most successful and feasible option for reforesting cutovers is natural regeneration with a mix of the three main tree species, but uncertainties remain about the temporal and spatial pattern of regeneration, changes in species composition, and the time required for stand establishment after cutting. Our study addressed these concerns by examining regeneration patterns on 6 sites that were clearcut 11-12 years prior to sampling and left to regenerate naturally. The sites were located at the lower limits of the zone in the Tetrahedron Range, near Sechelt, at elevations from 1060-1100m.

Hantaviruses are the causative agents of hemorrhagic fever with renal syndrome (HFRS) in Eurasia, and of hantavirus cardiopulmonary syndrome (HCPS) in the Americas. Transmission to humans usually occurs by inhalation of aerosolized virus-contaminated rodent excreta. To date, human-to-human transmission has only been described for the Andes hantavirus. The mode of transmission of Andes hantavirus is not yet known, but transmission through saliva has been suggested. In Sweden, we have one hantavirus that is pathogenic to humans, Puumala virus (PUUV), which is endemic in Central and Northern Europe. It induces a relatively mild form of HFRS, also called nephropathia epidemica (NE). The rodent reservoir is the bank vole (Myodes glareolus). The mechanism behind the pathogenesis of hantavirus is complex and probably involves both virus-mediated and host-mediated mechanisms. The aim of this project was to investigate the transmission mechanisms and pathogenesis of hantavirus disease in humans. In our first study, we described the largest outbreak of PUUV so far in Sweden. We investigated factors that might be important for causing the outbreak, and suggested that a peak in the bank vole population together with concurrent extreme weather conditions most probably contributed to the outbreak. Our next studies concentrated on human-to-human transmission of hantaviruses. We found PUUV RNA in saliva from PUUV-infected patients, suggesting that there is PUUV in the saliva of infected humans, although no person-to person transmission appears to occur with PUUV.  In the studies that followed, we showed that human saliva and human salivary components could inhibit hantavirus replication. We also found PUUV-specific IgA in the saliva of PUUV-infected patients, which might prevent person-to-person transmission of the virus.  In the final study, we focused on the pathogenesis of NE. One hundred five patients were included in a prospective study.  They were divided into a group with mild disease and a group with moderate or severe disease. We found that the immune response had a dual role in disease development. It was partly responsible for development of severe disease, with significantly higher amounts of neutrophils in severely ill patients, but it was also protective against severe disease, because patients with mild disease had higher levels of PUUV-specific IgG. In conclusion, a peak in the bank vole population in combination with extreme weather will increase the risk of human infection, PUUV RNA is present in saliva, PUUV-specific IgA and salivary components inhibit person-to-person transmission of PUUV, and the immune response is important for the pathogenesis of PUUV and the severity of the disease. / Hantavirus är en grupp av virus som finns hos gnagare som bär på viruset utan att själva bli märkbart sjuka. Varje hantavirus har anpassat sig till sin egen art av gnagare som de infekterar (kallas virusets reservoar). Hantaviruset kan överföras till människor från gnagare och kallas då för en zoonos eftersom detsprids från djur till människa. I människa orsakar hantavirus blödarfeber med njurpåverkan i Eurasien och blödarfeber med med hjärt och lungpåverkan i Nord- och Sydamerika. I Sverige har vi bara ett hantavirus som är sjukdomsframkallande hos människor, Puumala-viruset som även finns i delar av övriga Europa. Det framkallar en relativt mild form av blödarfeber, som kallas sorkfeber eller Nephropathia epidemica. Puumala-virusets reservoar är skogssorken (Myodes glareolus). Människor smittas oftast av hantavirus när de andas in infekterat damm som innehåller utsöndringar (avföring, urin eller saliv) från gnagare som har torkat in och sedan blivit luftburet. Vad man vet hittills så finns det bara ett hantavirus som smittar från person till person, för övriga hantavirus är människan en ”dead end”. Det virus som kan smitta från person till person heter Andes hantavirus och finns i Sydamerika. Andes hantavirus har en mus som reservoar från vilken människor kan smittas, sedan har smittan i vissa fall förts vidare från människa till människa, som tur är har dessa utbrott gått att stoppa. Fastän utbrotten har varit små har många personer dött, eftersom dödligheten är så hög, ungefär 30-40% av de diagnostiserade fallen dör. Hur Andes hantavirus överförs från människa till människa är inte känt men överföring genom saliv har föreslagits. Hur viruset ger upphov till sjukdom hos människa är inte klarlagt. Studier talar för att mekanismen bakom sjukdomsutvecklingen (den så kallade patogenesen) hos hantavirusorsakade blödarfebrar är komplex. Sannolikt beror patogenesen både på egenskaper hos viruset och värden d.v.s. människan som är smittad av viruset. Vårt mål med detta projekt var att undersöka vad som hindrar överföring av Puumala hantavirus från människa till människa och att undersöka hur virusinfektionen påverkar sjukdomsutvecklingen hos människan. I vår första studie beskrev vi det största utbrottet av sorkfeber hittills i Sverige och vi undersökte faktorer som kan ha orsakat utbrottet. Vi föreslog att en topp i skogssorkpopulationen samtidigt med extremt varmt väder troligen bidrog till utbrottet. Utbrottet skedde i december och det extremt varma vädret medförde att snön smälte bort. Sorkarna bor vanligtvis under snön på vintern, vi tror att frånvaro av snötäcke fick sorkarna att söka sig till byggnader för att söka skydd och där kom i kontakt med människor. Våra efterföljande studier fokuserade på överföring av hantavirus från människa till människa. Vi hittade Puumala-virusets arvsmassa (RNA) i saliv från sorkfeberpatienter, vilket tyder på att det finns Puumala-virus i saliven hos infekterade människor, även om ingen överföring från person till person verkar inträffa. I efterföljande studier visade vi att mänsklig saliv och mänskliga salivkomponenter minskar hantavirus smittsamhet. Vi fann också Puumala-virusspecifika IgA-antikroppar i saliven från sorkfeberpatienter, vilket kan förhindra överföring från person till person. I den sista studien fokuserade vi på patogenesen hos människor efter hantavirusinfektion. 105 patienter ingick i en prospektiv studie och delades in i en grupp med mild sjukdom och en grupp med måttlig/svår sjukdom. Vi hittade en dubbel roll hos immunsvaret för sjukdomsutvecklingen. Immunsvaret var delvis ansvarig för utveckling av svår sjukdom med betydligt högre mängd neutrofiler hos svårt sjuka patienter, men det var också skyddande mot allvarlig sjukdom, eftersom patienter med en mild sjukdom hade högre nivåer av Puumalavirusspecifika IgG-antikroppar. Detta talar för att behandling med IgG-antikroppar specifikt riktade mot hantavirus skulle kunna vara effektiv hos hantavirusinfekterade patienter. Sammanfattningsvis; en topp i skogssorkspopulationen i kombination med extremt väder ökar risken för infektion hos människor; Puumala-virus arvsmassa (RNA) finns i saliv; Puumala-virusspecifika IgA-antikroppar och salivkomponenter hämmar överföring av Puumalavirus från person till person; immunsvaret är viktigt för Puumala-virus patogenes och sjukdomens svårighetsgrad.

Cette thèse a pour objectif principal de contribuer à la compréhension des facteurs environnementaux agissant sur la diversité et la productivité des communautés végétales alpine, et dans un deuxième temps de mettre en évidence des changements récents dans la structure de la végétation dans un contexte tempéré alpin, les Alpes françaises. L’approche adoptée se base sur des méthodes issues de la télédétection et également de l’écologie végétale, en combinant des relevés de végétation avec les données de climat de l’imagerie à haute résolution. Dans le premier chapitre, je démontre l’intérêt de quantifier la durée d’enneigement afin de pouvoir prédire les patrons de diversité taxonomique et fonctionnelle, en montrant aussi que la modélisation spatiale de la productivité primaire reste un défi important dans le contexte des paysages alpins. Dans le deuxième chapitre, je teste l’utilité de l’imagerie satellitaire pour quantifier les conditions environnementales au niveau des communautés végétales, et je mets en évidence que l’habitat des communautés dominantes peut être différencié à l’échelle régionale par la date de déneigement et le pic en productivité. J’essaie également de voir si la diversité fonctionnelle influe sur la réponse NDVI dans le cadre de trois années de durée d’enneigement contrastées. Le troisième chapitre marque un changement d’approche, dans lequel je passe à l’analyse de la dynamique observée de la végétation pendant les dernières décennies dans deux sites : la Réserve Naturelle des Hauts Plateaux du Vercors (RNHPV) et le Parc National des Ecrins (PNE). L’analyse diachronique de l’écotone forêt-prairie dans la RNHPV montre une forte expansion de la forêt à Pinus uncinata pendant les soixante dernières années, en réponse à un réchauffement global et également des changements spatio-temporels dans les usages des terres en lien avec le pâturage. Dans la deuxième partie, je montre qu’avec les satellites on observe une tendance de verdissement à l’échelle du PNE pendant les dernières décennies. Je propose qu’une réduction dans la durée d’enneigement et un réchauffement depuis les années 1980s ont contribué à une augmentation de la productivité des canopées dans des contextes alpins de haute altitude, et ceci indépendamment des effets d’utilisation des terres. Pris ensemble, au lieu d’avancer un aspect précis de l’écologie alpine, mon travail sert à compléter nos connaissances du fonctionnement des communautés végétales alpines et à confirmer certaines hypothèses basées sur l’observation terrain avec des analyses spatiales robustes. / The central aim of this thesis is to contribute to current understanding of environmental drivers of plant diversity and productivity as well as of recent changes in vegetation structure in a temperate alpine context, the French Alps. My approach draws on methods from remote sensing and plant ecology by combining plot-based measures of plant diversity and climate data with high-resolution imagery. Chapter I demonstrates the importance of quantifying snow cover duration for predicting patterns of plant taxonomic and functional diversity, and also highlights the ongoing challenge of modeling spatial gross primary productivity dynamics in alpine landscapes. In Chapter II, I explore the utility of satellite imagery for quantifying environmental conditions experienced by alpine plant communities, and further show how metrics of snow cover duration and peak productivity can be used to differentiate habitat for dominant alpine plant communities. I also explore how functional diversity mediates NDVI responses to highly contrasting snow years. Chapter III provides new evidence of recent shifts occurring in high-elevation plant communities in the French Alps in response to climate and land-use change. Analysis of the forest-grassland ecotone in the Vercors Regional Park shows a strong dynamic of forest expansion in response to overall climate warming and local shifts in grazing-related land-use practices, which supports findings from other studies conducted elsewhere in the Alps and Pyrenees. In the second part of Chapter III, for the first time I present evidence of greening dynamics in a protected area of the French Alps, the Ecrins National Park. I propose that a decrease in snow cover duration and pronounced warming occurring in the 1980s likely contributed to increased canopy productivity in high alpine contexts, and are driving long-term greening in the absence of land-use change. Taken collectively, rather than pushing a specific aspect alpine ecology forward, my work helps to fill out our working knowledge of alpine plant communities and serves to solidify a number of field-based observations by carrying out robust spatial analyses.