@inbook{12650,
  abstract     = {Streamflow is a hydrological variable measured at a defined river cross-section; it spatially integrates the runoff generating processes in the contributing watershed, including precipitation and air temperature. Trends in streamflow are progressive changes in the time series of streamflow that can be detected with statistical methods and their statistical significance can be assessed. Mountainous regions are particularly vulnerable to streamflow change because of their high specific runoff and the sensitivity to the distribution of precipitation and air temperature, and the processes of snow accumulation and melt.},
  author       = {Molnar, Peter and Burlando, Paolo and Pellicciotti, Francesca},
  booktitle    = {Encyclopedia of Snow, Ice and Glaciers},
  editor       = {Singh, Vijay and Singh, Pratap and Haritashya, Umesh},
  isbn         = {978-90-481-2641-5},
  issn         = {1871-756X},
  pages        = {1084--1089},
  publisher    = {Springer Nature},
  title        = {{Streamflow Trends in Mountainous Regions}},
  doi          = {10.1007/978-90-481-2642-2_543},
  year         = {2011},
}