dc.contributor.author |
Panagoulia, Dionysia |
en |
dc.contributor.author |
Dimou, George |
en |
dc.date.accessioned |
2014-03-01T02:41:05Z |
|
dc.date.available |
2014-03-01T02:41:05Z |
|
dc.date.issued |
1995 |
en |
dc.identifier.issn |
01447815 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/30361 |
|
dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-0029516322&partnerID=40&md5=fc804b9b0fb5b47491499a9ebe71f8e2 |
en |
dc.subject |
Climate Change |
en |
dc.subject |
Climate Change Scenario |
en |
dc.subject |
Climatic Condition |
en |
dc.subject |
Hydrologic Model |
en |
dc.subject |
Soil Moisture |
en |
dc.subject |
Surface Runoff |
en |
dc.subject |
Water Resource Management |
en |
dc.subject |
Water Storage |
en |
dc.subject |
Goddard Institute for Space Studies |
en |
dc.subject |
National Weather Service |
en |
dc.subject.other |
Climate change |
en |
dc.subject.other |
Climatology |
en |
dc.subject.other |
Groundwater flow |
en |
dc.subject.other |
Management |
en |
dc.subject.other |
Mathematical models |
en |
dc.subject.other |
Moisture |
en |
dc.subject.other |
Precipitation (meteorology) |
en |
dc.subject.other |
Runoff |
en |
dc.subject.other |
Snow |
en |
dc.subject.other |
Soils |
en |
dc.subject.other |
Stream flow |
en |
dc.subject.other |
Hydrological models |
en |
dc.subject.other |
Mesochora catchments |
en |
dc.subject.other |
Snowmelt |
en |
dc.subject.other |
Soil moisture |
en |
dc.subject.other |
Water resources management |
en |
dc.subject.other |
Flow interactions |
en |
dc.title |
Groundwater-streamflow interactions under changing climate conditions |
en |
heal.type |
conferenceItem |
en |
heal.publicationDate |
1995 |
en |
heal.abstract |
The long-term groundwater-streamflow interactions of the medium-sized mountainous Mesochora catchment under changing climatology have been analysed. The climate changes were simulated through a set of hypothetical and monthly GISS (Goddard Institute for Space Studies) scenarios of temperature increases coupled with precipitation changes. Two catchment hydrological models were used: the snowmelt and soil moisture accounting models of the US National Weather Service River Forecast System (US NWSRFS). The groundwater was represented through the lower zone one-tension water storage and two free water storages parameterized by the soil moisture model, while the streamflow was the sum of direct runoff, surface runoff and interflow from the upper zone free water, as well as the primary and secondary base flows yielded by the model. The interactions between groundwater and streamflow was expressed by the ratio of the two variables on a monthly basis. Both sets of climate change scenarios resulted in moderate influence on groundwater-streamflow interaction during the winter months and in a very high one in the spring and summer months. This will probably have negative impacts on various problems of water resources management. |
en |
heal.publisher |
IAHS, Wallingford, United Kingdom |
en |
heal.journalName |
IAHS-AISH Publication |
en |
dc.identifier.issue |
230 |
en |
dc.identifier.spage |
191 |
en |
dc.identifier.epage |
196 |
en |