Understanding the relative role of dispersion mechanisms across basin scales
• We analyze dispersive contributions to hydrologic response through scales. • We consider an idealized basin with variable shape, drainage density and scale. • Kinematic dispersion counteracts geomorphological one for medium size basins. • Random variability of hillslope velocity adds positive kine...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Di Lazzaro, M. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Umfang: |
14 |
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| Übergeordnetes Werk: |
Enthalten in: Modeling sourcing strategies to mitigate part obsolescence - Shen, Yuelin ELSEVIER, 2014, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:91 ; year:2016 ; pages:23-36 ; extent:14 |
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| DOI / URN: |
10.1016/j.advwatres.2016.03.003 |
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| 520 | |a • We analyze dispersive contributions to hydrologic response through scales. • We consider an idealized basin with variable shape, drainage density and scale. • Kinematic dispersion counteracts geomorphological one for medium size basins. • Random variability of hillslope velocity adds positive kinematic dispersion. • Non-uniform runoff production yields an additional geomorphic dispersive term. | ||
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• We analyze dispersive contributions to hydrologic response through scales. • We consider an idealized basin with variable shape, drainage density and scale. • Kinematic dispersion counteracts geomorphological one for medium size basins. • Random variability of hillslope velocity adds positive kinematic dispersion. • Non-uniform runoff production yields an additional geomorphic dispersive term. |
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• We analyze dispersive contributions to hydrologic response through scales. • We consider an idealized basin with variable shape, drainage density and scale. • Kinematic dispersion counteracts geomorphological one for medium size basins. • Random variability of hillslope velocity adds positive kinematic dispersion. • Non-uniform runoff production yields an additional geomorphic dispersive term. |
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"><subfield code="a">• We analyze dispersive contributions to hydrologic response through scales. • We consider an idealized basin with variable shape, drainage density and scale. • Kinematic dispersion counteracts geomorphological one for medium size basins. • Random variability of hillslope velocity adds positive kinematic dispersion. • Non-uniform runoff production yields an additional geomorphic dispersive term.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zarlenga, A.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Volpi, E.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier Science</subfield><subfield code="a">Shen, Yuelin ELSEVIER</subfield><subfield code="t">Modeling sourcing strategies to mitigate part obsolescence</subfield><subfield code="d">2014</subfield><subfield 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