Download AVO Course Notes, Part 3. Poor AVO Utilization by Castagna J.P. PDF

By Castagna J.P.

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Extra resources for AVO Course Notes, Part 3. Poor AVO Utilization

Example text

A. Adaptations. . . . . . . . . . . . . . . . . . . . . B. Constrained Streams: EVects and Recovery . . . . . . . . . C. Response to Floods in Floodplain River Systems . . . . . . . V. The Human Dimension. . . . . . . . . . . . . . . . . . . VI. Conclusions. . . . . . . . . . . . . . . . . . . . . . . Acknowledgments . . . . . . . . . . . . . . . . . . . . . . . References . . .

2005). The seasonality of these rains is such that high runoV events occur almost exclusively in the summer half year in the Darling catchment (Moore, 1988), and mostly in winter in the more southern Murray catchment, although small subcatchments can experience high runoVs due to localized summer storms in the southern regions (Grimmer, 1988). II. INTERANNUAL VARIABILITY OF RAINFALL The large variability of Australian rainfall is due to variations in large‐scale influences including the El Nin˜o–Southern Oscillation (ENSO), the latitude of the westerlies and variations in standing wave patterns associated with blocking phenomena (Fig.

CSIRO Division of Atmospheric Research, Aspendale. ’’ CSIRO Division of Atmospheric Research, Aspendale. ’’ CSIRO Division of Atmospheric Research, Aspendale. L. (1953) Climatic changes in Australia since 1880. Aust. J. Phys. 6, 209–218. B. L. ’’ Water 2000: Consultants Report 11, AGPS, Canberra. Emanuel, K. (2005a) Increasing destructiveness of tropical cyclones over the past 30 years. Nature 436, 686–688. Emanuel, K. (2005b) Emanuel replies. 04427. M. J. (1995) Potential impacts of global warming on the frequency and magnitude of heavy precipitation.

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