Groundwater and Surface Water Modelling
Course, Master's level, 1HY041
Expand the information below to show details on how to apply and entry requirements.
Spring 2027 Spring 2027, Uppsala, 67%, On-campus, English
- Location
- Uppsala
- Pace of study
- 67%
- Teaching form
- On-campus
- Instructional time
- Daytime
- Study period
- 22 March 2027–6 June 2027
- Language of instruction
- English
- Entry requirements
-
120 credits with 90 credits in earth science or in technology or physics. 15 credits mathematics. Participation in course Hydrological Processes, of which 3 credits must be completed. Proficiency in English equivalent to the Swedish upper secondary course English 6.
- Selection
-
Higher education credits in science and engineering (maximum 240 credits)
- Fees
- If you are not a citizen of a European Union (EU) or European Economic Area (EEA) country, or Switzerland, you are required to pay application and tuition fees.
- First tuition fee instalment: SEK 27,500
- Total tuition fee: SEK 27,500
- Application deadline
- 15 October 2026
- Application code
- UU-68300
Admitted or on the waiting list?
- Registration period
- 8 March 2027–21 March 2027
- Information on registration from the department
Spring 2027 Spring 2027, Uppsala, 67%, On-campus, English For exchange students
- Location
- Uppsala
- Pace of study
- 67%
- Teaching form
- On-campus
- Instructional time
- Daytime
- Study period
- 22 March 2027–6 June 2027
- Language of instruction
- English
- Entry requirements
-
120 credits with 90 credits in earth science or in technology or physics. 15 credits mathematics. Participation in course Hydrological Processes, of which 3 credits must be completed. Proficiency in English equivalent to the Swedish upper secondary course English 6.
Admitted or on the waiting list?
- Registration period
- 8 March 2027–21 March 2027
- Information on registration from the department
About the course
The course provides you with an understanding of the processes and mathematical tools necessary for the quantification of water flow and availability in different parts of the hydrological cycle, with a special focus on groundwater and surface water. A large emphasis is placed on exercises with existing numerical models.