@misc{weichselgartner_the_2002_2011, 
author={Weichselgartner, J., Breviere, E.},
title={The 2002 Flood Disaster in the Elbe Region, Germany: A Lack of Context-Sensitive Knowledge},
year={2011},
howpublished = {book part},
abstract = {The unusual intensity of rain exceeded the soil’s capacity to retain water and generated two types of floods in the Elbe river basin: flash floods at the tributaries of mountainous catchments (e.g., Weißeritz River, Upper Mulde River) with high discharge dynamic and flow velocity, and slow swell floods of the Elbe River and the lower reach of its main tributaries (e.g., Vltava River, Joint Mulde River). In the Saxon capital of Dresden, the Elbe River rose from a normal summer level of about 2 m, surpassing the historical flood mark of 8.77 m seen in March 1845, to reach a water level of 9.40 m – the highest level ever been recorded.},
note = {Weichselgartner, J.; Breviere, E.: The 2002 Flood Disaster in the Elbe Region, Germany: A Lack of Context-Sensitive Knowledge. In: Allen, B.; Dowty, R. (Ed.): Dynamics of Disaster: Lessons on Risk, Response, and Recovery. London ; Washington, DC: Earthscan. 2011. 141-158.}}