Abstract
Unlike hydrometeorology, which focuses on short-term interactions of the atmosphere and hydrosphere, hydroclimatology analyzes such interactions on broader spatial and temporal scales. Hirschboeck utilizes the context of hydroclimatology to re-evaluate various assumptions and models that are presently used to describe how floods vary over time in relation to climate. -from Editors
Original language | English (US) |
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Pages (from-to) | 27-49 |
Number of pages | 23 |
Journal | Unknown Journal |
State | Published - 1988 |
Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences