Next Article in Journal
A Comparative Analysis of Runoff and Soil Loss Characteristics between “Extreme Precipitation Year” and “Normal Precipitation Year” at the Plot Scale: A Case Study in the Loess Plateau in China
Previous Article in Journal
Quantification of Fog Water Collection in Three Locations of Tenerife (Canary Islands)
Article Menu

Export Article

Open AccessArticle
Water 2015, 7(7), 3320-3342; doi:10.3390/w7073320

Runoff Response to Climate Warming and Forest Disturbance in a Mid-Mountain Basin

1,* , 1,†
Faculty of Science, Charles University in Prague, Albertov 6, Prague 2, 128 43, Czech Republic
DHI a.s., Na Vrsich 5, Prague 10 100 00, Czech Republic
These authors contributed equally to this work.
Author to whom correspondence should be addressed.
Academic Editor: Miklas Scholz
Received: 27 March 2015 / Revised: 11 June 2015 / Accepted: 18 June 2015 / Published: 26 June 2015
View Full-Text   |   Download PDF [2946 KB, uploaded 26 June 2015]   |  


A headwater basin in the Sumava Mountains (Czech Republic), the upper Vydra basin, has undergone forest disturbance as a result of repeated windstorms, a bark beetle outbreak, and forest management. This study analyzed the long-term (1961–2010) hydro-climatic changes by using a combination of statistical analyses, including Mann-Kendall tests, CUSUM analysis, Buishand’s and Petitt’s homogeneity tests, and Kriging. Although the runoff balance over the study period experienced no apparent changes due to climate warming and forest disturbance, significant changes were detected in the share of direct runoff and baseflow, intra-annual variability of the runoff regime, seasonal runoff patterns, and the distribution of peak and low flow events. The seasonal runoff substantially shifted from summers (decreased from 40% to 28%) to springs (increased by 10%). The occurrence of peak flow events has doubled since the 1980s, with a seasonal shift from late spring towards the early spring, while the occurrence of low-flow days decreased by two-thirds. By 1990, these changes were followed by a seasonal shift in runoff from autumn to mid-winter. The changes in hydrological regime in the mid-mountain basin indicate the sensitivity of its hydrological system and the complexity of its feedback with the changing environment. View Full-Text
Keywords: runoff variability; baseflow; peak flows; low flows; climate warming; forest disturbance runoff variability; baseflow; peak flows; low flows; climate warming; forest disturbance

Figure 1

This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).

Supplementary material

Scifeed alert for new publications

Never miss any articles matching your research from any publisher
  • Get alerts for new papers matching your research
  • Find out the new papers from selected authors
  • Updated daily for 49'000+ journals and 6000+ publishers
  • Define your Scifeed now

SciFeed Share & Cite This Article

MDPI and ACS Style

Langhammer, J.; Su, Y.; Bernsteinová, J. Runoff Response to Climate Warming and Forest Disturbance in a Mid-Mountain Basin. Water 2015, 7, 3320-3342.

Show more citation formats Show less citations formats

Related Articles

Article Metrics

Article Access Statistics



[Return to top]
Water EISSN 2073-4441 Published by MDPI AG, Basel, Switzerland RSS E-Mail Table of Contents Alert
Back to Top