As extraction techniques are improving an increased number of low grade deposits can be economically mined. However, this also means that the number of open pit mines will increase and as a result the number of pit lakes as well. This is of environmental concern as the pit lakes, depending on the geology and other factors, potentially can have a negative impact on surrounding ecosystems, e.g. through high metal concentrations, low pH, and by affecting the hydrologic system. Sweden has a long history of mining and is one the largest metal suppliers in Europe, and many of the mines are located in the northern part of the country. The project aim was to better understand and be able to predict pit lake water quality and some of the underlying processes affecting it, with a focus on cold climates, where temperatures are low and the lakes are ice covered for prolonged periods of time.  The following field measurements were conducted in the Laver and Åkerberg pit lakes: 1) minewall stations measuring metal leaching rates from pit walls, 2) oxygen and hydrogen isotopic composition of precipitation and pit lakes to better understand pit lake hydrology (including also the Udden and Rävlidmyran pit lakes), 3) a nutrient limitation and metal uptake experiment in the Åkerberg pit lake, and 4) a continuously measuring buoy installed in the Laver pit lake where short term fluctuations in water quality parameters could be observed. A bathymetric map of the Åkerberg pit lake was also generated during the project. Additionally, modelling of the Rävlidmyran pit lake was conducted based on three different climate scenarios. Measurements of water quality parameters showed that both the Laver and Åkerberg pit lakes have relatively good water quality, pH 6.1–7.4, specific conductivity 41–352 μS/cm and pH 7.6-7.7, specific conductivity 137–140 μS/cm, respectively, and low concentrations of metals. Algal growth was successfully stimulated in microcosms in the Åkerberg pit lake, through addition of the nutrients N and P in combination. Chlorophyll-a concentrations, which were used to estimate algal growth, were 9.5-11 times higher than at the beginning of the experiment in these microcosms. It was also seen that the metal concentration in the suspended particulate phase increased, suggesting that metals were taken up by algae. In the Laver pit lake measurements from the continuously measuring buoy showed diurnal variations for pH, dissolved oxygen, and temperature. The pH and dissolved oxygen was increasing during daytime, indicating that algal growth was increasing. A local meteoric water line, which can be used to separate sources of water from precipitation, if their isotopic compositions are different, was constructed for the study area (δ2H = (7.80 ± 0.09) δ18O + (4.35 ± 1.35) ‰). It was seen that the groundwater had a similar stable isotopic composition as precipitation, as its composition fell on the local meteoric water line. It was also seen that the studied pit lakes had undergone evaporation as they plotted on a local evaporation line (δ2H = (6.88 ± 0.47) δ18O + (−12.75 ± 5.60) ‰). Residence times were calculated for the pit lakes, ranging from 2.9-44.9 years, using the isotopic mass balance method. Modelling of the Rävlidmyran pit lake suggests that it is fairly stable and will remain meromictic during a modelled 100 year period. No major differences in redox or oxygen levels were observed. The temperature is predicted to increase in the mixolimnion along with a slight decrease in dissolved oxygen concentration. The modelling also indicates that the water outflow from the lake might increase, and as a consequence, a slight increase of metal outflow was observed as well.  Based on minewall stations, installed at the Laver and Åkerberg mine sites, leaching rates (µg/m2/week) of metals were estimated. These were used to approximate the total contribution of metals from the pit walls to the pit lakes over the course of a year. A difference in metal leaching could be observed for the two mine sites which could be attributed to the deposit type.