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(1 Jan–31 Dec 2008) for the verification domain over the Northern Hemisphere. The year 2008 is chosen because it is included in the Year of Tropical Convection (YOTC) period. YOTC data explicitly contain diabatic forcing terms ( Waliser and Moncrieff 2008 ), and follow-up studies that focus in more detail on the physical processes responsible for the forecast errors are possible. A 1-yr forecast error climatology was produced by comparing output from the IFS model at five different forecast lead
(1 Jan–31 Dec 2008) for the verification domain over the Northern Hemisphere. The year 2008 is chosen because it is included in the Year of Tropical Convection (YOTC) period. YOTC data explicitly contain diabatic forcing terms ( Waliser and Moncrieff 2008 ), and follow-up studies that focus in more detail on the physical processes responsible for the forecast errors are possible. A 1-yr forecast error climatology was produced by comparing output from the IFS model at five different forecast lead
-based short-range QPF evaluation over Switzerland . Meteor. Z. , 17 , 827 – 848 , doi:10.1127/0941-2948/2008/0344 . Johnson, C. , and Swinbank R. , 2009 : Medium-range multimodel ensemble combination and calibration . Quart. J. Roy. Meteor. Soc. , 135A , 777 – 794 , doi:10.1002/qj.383 . Kiladis, G. N. , and Weickmann K. M. , 1992 : Extratropical forcing of tropical Pacific convection during winter . Mon. Wea. Rev. , 120 , 1924 – 1938 . Klein, H. , and Coauthors , 2010 : Saharan
-based short-range QPF evaluation over Switzerland . Meteor. Z. , 17 , 827 – 848 , doi:10.1127/0941-2948/2008/0344 . Johnson, C. , and Swinbank R. , 2009 : Medium-range multimodel ensemble combination and calibration . Quart. J. Roy. Meteor. Soc. , 135A , 777 – 794 , doi:10.1002/qj.383 . Kiladis, G. N. , and Weickmann K. M. , 1992 : Extratropical forcing of tropical Pacific convection during winter . Mon. Wea. Rev. , 120 , 1924 – 1938 . Klein, H. , and Coauthors , 2010 : Saharan
