Hidrológiai Közlöny 2009 (89. évfolyam)

2. szám - Gribovszki Zoltán–Kalicz Péter–Szilágyi József: Napi periódusú ingadozás a hidrológiai jellemzőkben

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Water Supply Paper 659-A., 1932. Wicht, C. L.: Diumal fluctuation in jonkershoeckstreams due to evapo­ration and transpiration. J.S. African For. Ass. , 7:34-49, 1941. Wicht, C. L.: Depletion of ground water flow in jonkershoeck streams. J. S. African For. Ass., 8:50-63, 1942. Zsuffa István: Műszaki Hidrológia I-IV. kötet. Műegyetemi Kiadó, 1996-99. ISBN 963-420-493-7. A kézirat beérkezett: 2008. október 9-én GRIBOVSZKI ZOLTÁN PhD, okleveles erdőmérnök, egyetemi szakmérnök, vízépítő, vízkészletfeltárás, vízrajz, egyetemi docens (Nyugat-ma­gyarországi Egyetem, Erdőmérnöki Kar, Geomatikai, Erdőfeltárási és Vízgazdálkodási Intézet). KALICZ PÉTER PhD, okleveles környezetmérnök, egyetemi adjunktus (Nyugat-magyarországi Egyetem, Erdőmérnöki Kar, Geomati­kai, Erdőfeltárási és Vízgazdálkodási Intézet). SZILAGYI JÓZSEF az MTA doktora, okleveles meteorológus, hidrológiai MSc (Nem Hampshire-i Egyetem), PhD (Kaliforniai Egyetem), egyetemi tanár (Budapesti Műszaki és Gazdaságtudományi Egyetem). Diurnal fluctuation of hydrological variables Gribovszki, Z. - Kalicz, P. - Szilágyi, J. Abstract: Diumal fluctuations of hydrological variables (e.g., shallow groundwater level or streamflow rate) are relatively rarely investigated in the hydrologic literature although these short-term fluctuations may incorporate useful information for the characterization of hydro-ecological systems. The fluctuations can be induced by several factors like the (a) alternating processes of freezing and melting; (b) early afternoon rainfall events in the tropics; (c) changing of the streambed hydra­ulic conductivity triggered by temperature variations, and; (d) diumal cycle of water uptake by the vegetation. In tempe­rate climates, one of the most important diumal fluctuation-inducing factors is the water consumption of vegetation, the­refore a detailed overview is provided on the history of such research. Beside a systematic categorization of the relevant historical research, models that calculate local or catchment-scale groundwater evapotranspiration from diumal fluctuati­ons of groundwater level and/or streamflow rate have been reviewed. Compared to traditional evapotranspiration calcu­lation methods these approaches may excel in that they generally employ a small number of parameters and/or variables to measure, are typically simple to use, and yet can yield results even on a short time-scale (i.e., hours). While, e.g., tem­perature-based methods of evapotranspiration are simple too, they cannot be applied or become inaccurate over shorter time periods. Similarly, traditional approaches (such as eddy correlation or Bowen ratio based) are accurate for shorter time steps but they require a number of measurable input variables. Keywords: diurnal fluctuation, groundwater, streamflow, evapotranspiration

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