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  • Peter J. Lamb Special Collection: Climate Variability and Its Impacts x
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Robert A. Clark III, Zachary L. Flamig, Humberto Vergara, Yang Hong, Jonathan J. Gourley, Daniel J. Mandl, Stuart Frye, Matthew Handy, and Maria Patterson

the development of new hydrological modeling software: EF5. EF5 is a framework encompassing multiple hydrological model cores, including but not limited to the grid cell–based water balance component of CREST, linear reservoir routing as implemented in CREST, routing using the kinematic wave assumption ( Chow et al. 1988 ), and the Sacramento family of water balance models ( Burnash et al. 1973 ). EF5 accepts the same input file formats as the CREST model and adds support for GeoTIFF (tagged image

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Abdou L. Dieng, Saidou M. Sall, Laurence Eymard, Marion Leduc-Leballeur, and Alban Lazar

structures and their role in influencing tropical cyclogenesis . Mon. Wea. Rev. , 138 , 1399 – 1419 , doi: 10.1175/2009MWR2760.1 . 10.1175/2009MWR2760.1 Janiga , M. A. , and C. D. Thorncroft , 2013 : Regional differences in the kinematic and thermodynamic structure of African easterly waves . Quart. J. Roy. Meteor. Soc. , 139 , 1598 – 1614 , doi: 10.1002/qj.2047 . 10.1002/qj.2047 Kiladis , G. , C. Thorncroft , and N. Hall , 2006 : Three-dimensional structure and dynamics of African

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Elinor R. Martin and Chris Thorncroft

, 2468 – 2483 , doi: 10.1175/JCLI4139.1 . Hopsch , S. B. , C. D. Thorncroft , and K. R. Tyle , 2010 : Analysis of African easterly wave structures and their role in influencing tropical cyclogenesis . Mon. Wea. Rev. , 138 , 1399 – 1419 , doi: 10.1175/2009MWR2760.1 . Janiga , M. A. , and C. D. Thorncroft , 2013 : Regional differences in the kinematic and thermodynamic structure of African easterly waves . Quart. J. Roy. Meteor. Soc. , 139 , 1598 – 1614 , doi: 10.1002/qj.2047 . Ji

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M. Issa Lélé, Lance M. Leslie, and Peter J. Lamb

, observations reveal a significant interannual variability in moisture transport. Drought years are generally associated with large decreases in moisture content in the low-level due to the weakening of the southwesterly flow, a much farther southward extent of moisture across WA, and a southward ITF position compared to its long-term average latitude. This is in agreement with Lamb (1978a) , who also found that during a DRY regime the tropical Atlantic near-equatorial trough, the kinematic axis, and the

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