scholarly journals Automation and human expertise in operational river forecasting

2016 ◽  
Vol 3 (5) ◽  
pp. 692-705 ◽  
Author(s):  
Thomas C. Pagano ◽  
Florian Pappenberger ◽  
Andrew W. Wood ◽  
Maria-Helena Ramos ◽  
Anders Persson ◽  
...  
Keyword(s):  
1979 ◽  
Vol 15 (6) ◽  
pp. 1823-1832 ◽  
Author(s):  
R. Uwe Jettmar ◽  
G. Kenneth Young ◽  
Richard K. Farnsworth ◽  
John C. Schaake
Keyword(s):  

1997 ◽  
Vol 25 ◽  
pp. 367-370 ◽  
Author(s):  
Richard Kattelmann

Snow cover in the intermittent snow zone of the Sierra Nevada can occupy more than 10 000 km2 of the mountain range, but it has received relatively little attention in river forecasting. Snow is deposited at lower elevations only during the cold storms of winter, and remains there only for a few days or weeks. When cold storms have created a thin snow cover at low elevations, a subsequent warm storm can melt this snow in just a few hours and increase the runoff response dramatically. Operational hydrological models and river-forecasting procedures have tended to overlook contributions from the intermittent-snow zone, focusing instead on rainfall-runoff or melt from the snowpack zone at higher elevations. Data-collection efforts are minimal in this zone, too. Ideally, spatially distributed models of snowmelt and runoff generation are needed to account for the typically large differences in snow cover on different aspects in the intermittent snow zone. Although aircraft and satellite imagery would be most desirable to monitor the distribution of snow cover in the intermittent-snow zone, even a few climate stations that report precipitation type and snow presence would be a major improvement over the present situation in the Sierra Nevada.


2012 ◽  
Vol 36 (4) ◽  
pp. 480-513 ◽  
Author(s):  
Robert J. Abrahart ◽  
François Anctil ◽  
Paulin Coulibaly ◽  
Christian W. Dawson ◽  
Nick J. Mount ◽  
...  

2009 ◽  
Vol 90 (6) ◽  
pp. 779-784 ◽  
Author(s):  
Julie Demargne ◽  
Mary Mullusky ◽  
Kevin Werner ◽  
Thomas Adams ◽  
Scott Lindsey ◽  
...  

Author(s):  
Faisal Hossain ◽  
A. H. Siddique-E-Akbor ◽  
Liton Chandra Mazumder ◽  
Sardar M. ShahNewaz ◽  
Sylvain Biancamaria ◽  
...  

2013 ◽  
Vol 10 (1) ◽  
pp. 145-187 ◽  
Author(s):  
N. J. Mount ◽  
C. W. Dawson ◽  
R. J. Abrahart

Abstract. In this paper we address the difficult problem of gaining an internal, mechanistic understanding of a neural network river forecasting (NNRF) model. Neural network models in hydrology have long been criticised for their black-box character, which prohibits adequate understanding of their modelling mechanisms and has limited their broad acceptance by hydrologists. In response, we here present a new, data-driven mechanistic modelling (DDMM) framework that incorporates an evaluation of the legitimacy of a neural network's internal modelling mechanism as a core element in the model development process. The framework is exemplified for two NNRF modelling scenarios, and uses a novel adaptation of first order, partial derivate, relative sensitivity analysis methods as the means by which each model's mechanistic legitimacy is explored. The results demonstrate the limitations of standard, goodness-of-fit validation procedures applied by NNRF modellers, by highlighting how the internal mechanisms of complex models that produce the best fit scores can have much lower legitimacy than simpler counterparts whose scores are only slightly inferior. The study emphasises the urgent need for better mechanistic understanding of neural network-based hydrological models and the further development of methods for elucidating their mechanisms.


1997 ◽  
Vol 25 ◽  
pp. 367-370 ◽  
Author(s):  
Richard Kattelmann

Snow cover in the intermittent snow zone of the Sierra Nevada can occupy more than 10 000 km2of the mountain range, but it has received relatively little attention in river forecasting. Snow is deposited at lower elevations only during the cold storms of winter, and remains there only for a few days or weeks. When cold storms have created a thin snow cover at low elevations, a subsequent warm storm can melt this snow in just a few hours and increase the runoff response dramatically. Operational hydrological models and river-forecasting procedures have tended to overlook contributions from the intermittent-snow zone, focusing instead on rainfall-runoff or melt from the snowpack zone at higher elevations. Data-collection efforts are minimal in this zone, too. Ideally, spatially distributed models of snowmelt and runoff generation are needed to account for the typically large differences in snow cover on different aspects in the intermittent snow zone. Although aircraft and satellite imagery would be most desirable to monitor the distribution of snow cover in the intermittent-snow zone, even a few climate stations that report precipitation type and snow presence would be a major improvement over the present situation in the Sierra Nevada.


Sign in / Sign up

Export Citation Format

Share Document