Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins
<p>Catchment-scale hydrological studies on drylands are lacking because of the scarcity of consistent data: observations are often available at the plot scale, but their relevance for the catchment scale remains unclear. A database of 24 years of stream gauge discharge and homogeneous high-res...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2019-06-01
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| Series: | Hydrology and Earth System Sciences |
| Online Access: | https://www.hydrol-earth-syst-sci.net/23/2665/2019/hess-23-2665-2019.pdf |
| _version_ | 1811234797089980416 |
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| author | D. Zoccatelli F. Marra M. Armon Y. Rinat J. A. Smith E. Morin |
| author_facet | D. Zoccatelli F. Marra M. Armon Y. Rinat J. A. Smith E. Morin |
| author_sort | D. Zoccatelli |
| collection | DOAJ |
| description | <p>Catchment-scale hydrological studies on drylands are lacking because of the
scarcity of consistent data: observations are often available at the plot
scale, but their relevance for the catchment scale remains unclear. A
database of 24 years of stream gauge discharge and homogeneous
high-resolution radar data over the eastern Mediterranean allows us to describe the properties of floods over catchments spanning from desert to
Mediterranean climates, and we note that the data set is mostly of moderate
intensity floods. Comparing two climatic regions, desert and Mediterranean,
we can better identify specific rainfall-runoff properties. Despite the large differences in rainfall forcing between the two regions, the resulting unit
peak discharges and runoff coefficients are comparable. Rain depth and
antecedent conditions are the most important properties to shape flood
response in Mediterranean areas. In deserts, instead, storm core properties
display a strong correlation with unit peak discharge and, to a lesser extent,
with runoff coefficient. In this region, an inverse correlation with mean
catchment annual precipitation suggests also a strong influence of local
surface properties. Preliminary analyses suggest that floods in catchments
with wet headwater and dry lower section are more similar to desert
catchments, with a strong influence of storm core properties on runoff
generation.</p> |
| first_indexed | 2024-04-12T11:41:21Z |
| format | Article |
| id | doaj.art-e3b21c91dc5746fbb276eceda332a5e0 |
| institution | Directory Open Access Journal |
| issn | 1027-5606 1607-7938 |
| language | English |
| last_indexed | 2024-04-12T11:41:21Z |
| publishDate | 2019-06-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Hydrology and Earth System Sciences |
| spelling | doaj.art-e3b21c91dc5746fbb276eceda332a5e02022-12-22T03:34:38ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382019-06-01232665267810.5194/hess-23-2665-2019Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basinsD. Zoccatelli0F. Marra1M. Armon2Y. Rinat3J. A. Smith4E. Morin5Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, IsraelInstitute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, IsraelInstitute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, IsraelInstitute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, IsraelDepartment of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey, USAInstitute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel<p>Catchment-scale hydrological studies on drylands are lacking because of the scarcity of consistent data: observations are often available at the plot scale, but their relevance for the catchment scale remains unclear. A database of 24 years of stream gauge discharge and homogeneous high-resolution radar data over the eastern Mediterranean allows us to describe the properties of floods over catchments spanning from desert to Mediterranean climates, and we note that the data set is mostly of moderate intensity floods. Comparing two climatic regions, desert and Mediterranean, we can better identify specific rainfall-runoff properties. Despite the large differences in rainfall forcing between the two regions, the resulting unit peak discharges and runoff coefficients are comparable. Rain depth and antecedent conditions are the most important properties to shape flood response in Mediterranean areas. In deserts, instead, storm core properties display a strong correlation with unit peak discharge and, to a lesser extent, with runoff coefficient. In this region, an inverse correlation with mean catchment annual precipitation suggests also a strong influence of local surface properties. Preliminary analyses suggest that floods in catchments with wet headwater and dry lower section are more similar to desert catchments, with a strong influence of storm core properties on runoff generation.</p>https://www.hydrol-earth-syst-sci.net/23/2665/2019/hess-23-2665-2019.pdf |
| spellingShingle | D. Zoccatelli F. Marra M. Armon Y. Rinat J. A. Smith E. Morin Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins Hydrology and Earth System Sciences |
| title | Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins |
| title_full | Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins |
| title_fullStr | Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins |
| title_full_unstemmed | Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins |
| title_short | Contrasting rainfall-runoff characteristics of floods in desert and Mediterranean basins |
| title_sort | contrasting rainfall runoff characteristics of floods in desert and mediterranean basins |
| url | https://www.hydrol-earth-syst-sci.net/23/2665/2019/hess-23-2665-2019.pdf |
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