{"language":[{"iso":"eng"}],"place":"Dordrecht","_id":"12650","date_updated":"2023-02-20T10:35:28Z","article_processing_charge":"No","editor":[{"first_name":"Vijay","last_name":"Singh","full_name":"Singh, Vijay"},{"full_name":"Singh, Pratap","last_name":"Singh","first_name":"Pratap"},{"full_name":"Haritashya, Umesh","last_name":"Haritashya","first_name":"Umesh"}],"scopus_import":"1","date_created":"2023-02-20T08:18:07Z","extern":"1","author":[{"full_name":"Molnar, Peter","first_name":"Peter","last_name":"Molnar"},{"last_name":"Burlando","first_name":"Paolo","full_name":"Burlando, Paolo"},{"id":"b28f055a-81ea-11ed-b70c-a9fe7f7b0e70","full_name":"Pellicciotti, Francesca","last_name":"Pellicciotti","first_name":"Francesca"}],"publication":"Encyclopedia of Snow, Ice and Glaciers","publication_status":"published","month":"07","doi":"10.1007/978-90-481-2642-2_543","alternative_title":["Encyclopedia of Earth Sciences Series"],"publication_identifier":{"isbn":["978-90-481-2641-5"],"eissn":["1871-756X"],"eisbn":["978-90-481-2642-2"],"issn":["1388-4360"]},"quality_controlled":"1","date_published":"2011-07-01T00:00:00Z","publisher":"Springer Nature","abstract":[{"text":"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.","lang":"eng"}],"oa_version":"None","day":"01","citation":{"ieee":"P. Molnar, P. Burlando, and F. Pellicciotti, “Streamflow Trends in Mountainous Regions,” in Encyclopedia of Snow, Ice and Glaciers, 1st ed., V. Singh, P. Singh, and U. Haritashya, Eds. Dordrecht: Springer Nature, 2011, pp. 1084–1089.","short":"P. Molnar, P. Burlando, F. Pellicciotti, in:, V. Singh, P. Singh, U. Haritashya (Eds.), Encyclopedia of Snow, Ice and Glaciers, 1st ed., Springer Nature, Dordrecht, 2011, pp. 1084–1089.","apa":"Molnar, P., Burlando, P., & Pellicciotti, F. (2011). Streamflow Trends in Mountainous Regions. In V. Singh, P. Singh, & U. Haritashya (Eds.), Encyclopedia of Snow, Ice and Glaciers (1st ed., pp. 1084–1089). Dordrecht: Springer Nature. https://doi.org/10.1007/978-90-481-2642-2_543","ama":"Molnar P, Burlando P, Pellicciotti F. Streamflow Trends in Mountainous Regions. In: Singh V, Singh P, Haritashya U, eds. Encyclopedia of Snow, Ice and Glaciers. 1st ed. Dordrecht: Springer Nature; 2011:1084-1089. doi:10.1007/978-90-481-2642-2_543","chicago":"Molnar, Peter, Paolo Burlando, and Francesca Pellicciotti. “Streamflow Trends in Mountainous Regions.” In Encyclopedia of Snow, Ice and Glaciers, edited by Vijay Singh, Pratap Singh, and Umesh Haritashya, 1st ed., 1084–89. Dordrecht: Springer Nature, 2011. https://doi.org/10.1007/978-90-481-2642-2_543.","ista":"Molnar P, Burlando P, Pellicciotti F. 2011.Streamflow Trends in Mountainous Regions. In: Encyclopedia of Snow, Ice and Glaciers. Encyclopedia of Earth Sciences Series, , 1084–1089.","mla":"Molnar, Peter, et al. “Streamflow Trends in Mountainous Regions.” Encyclopedia of Snow, Ice and Glaciers, edited by Vijay Singh et al., 1st ed., Springer Nature, 2011, pp. 1084–89, doi:10.1007/978-90-481-2642-2_543."},"status":"public","edition":"1","year":"2011","title":"Streamflow Trends in Mountainous Regions","page":"1084-1089","user_id":"2DF688A6-F248-11E8-B48F-1D18A9856A87","type":"book_chapter"}