Vis enkel innførsel

dc.contributor.authorGrythe, Karl Kristian
dc.contributor.authorGao, Yukun
dc.date.accessioned2010-11-30T12:11:18Z
dc.date.available2010-11-30T12:11:18Z
dc.date.issued2010
dc.identifier.urihttp://hdl.handle.net/11250/137486
dc.descriptionMasteroppgave i informasjons- og kommunikasjonsteknologi 2010 – Universitetet i Agder, Grimstaden_US
dc.description.abstractMeteorological and hydrological forecasts are very important to human’s life which concerns agriculture, industry, transport, etc. The Nordic hydropower industry use and develop hydrological forecasting models to make predictions of rivers steam flow. The quantity of incoming stream flow is important to the electricity production because excessive water in reservoir will cause flood and the loss of hydropower energy. Therefore the accurate prediction will help the managers decide the optimal production level in the reservoir at the current time. If for instance the predicted runoff exceeds the limit of water that the plant can process, then it is possible to increase production early so the water level does not get higher than the edge of the reservoir. In our project, we are studying the uncertainties which come from both meteorological and hydrological forecasting systems, and propose a new error correction methodology to reduce the uncertainties in the forecasted runoff. We study the uncertainties in the meteorological data, and then evaluate the accuracy of the meteorological data. Then we feed the meteorological data into a hydrological forecasting system, called the “OHBV model” with forecasted meteorological data. Later we run the model again with observed meteorological data. By running the model twice with different input we evaluate the performance of the OHBV model, and find the level of improvement expected when having a more accurate weather forecast. The OHBV model is also referred to as “OHBV” for short. At last we focus on error correction that are algorithms used to improve the runoff forecast based on statistics. We test the existing error correction method, called the “Powel algorithm”, and we identify how much of the error it could reduce. The error reduction is found by comparing the runoff forecast with the observation of stream flow runoff. Furthermore, we propose our own error correction method, referred to as “Yukun&Karl algorithm”, and finally evaluate the performance of the new method. Our results show that the main part of the error comes from the HBV model in the first forecast, while when using observation data as input into the model the output improves most for last days where the weather forecasts have higher uncertainty. Weather forecasts have errors, but have gone through much refinement the latest years, and until the HBV model performs better, this is not where the main focus should be. Since the OHBV model give high errors even in the prediction with the least of uncertainty (in the 1 day ahead in forecast), this should be investigated and improved. Error correction algorithms are applied after the model itself, and are used to give an overall improvement, though it sometimes can make the individual error larger. The best improvement by correction is in the “1 day ahead “runoff forecast, but after 4-5 days the Powel correction generally causes more errors than it can correct. The developed “Yukun&Karl algorithm” works up until the 8th day. The error corrections algorithms counter some of the effects from the simplification of hydrological systems in the OHBV model, but error correction is only based on the statistics of the input forecast. Error correction is a quick and relative simple way to improve the forecast, but as any “quick fix” it has its limitations, and can only improve forecasts some. The findings can result in further development of error correction and improve the prediction of runoff. Error correction can also be used in other fields, as long as the data used have statistical probabilities that can be exploiteden_US
dc.language.isoengen_US
dc.publisherUniversity of Agderen_US
dc.titleUncertainty analysis of hydro-meteorological forecastsen_US
dc.typeMaster thesisen_US
dc.source.pagenumber72en_US


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

Vis enkel innførsel