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effects on soil reflectance. Soil Sci. Amer. J. , 66 , 722 – 727 . Mahrt , L. , and M. Ek , 1984 : The influence of atmospheric stability on potential evaporation. J. Climate Appl. Meteor. , 23 , 222 – 234 . Mann , J. , and D. H. Lenschow , 1994 : Errors in airborne flux measurements. J. Geophys. Res. , 99 , 14519 – 14526 . Mitchell , K. E. , and Coauthors , 2004 : The multi-institution North American Land Data Assimilation System (NLDAS): Utilizing multiple GCIP products
effects on soil reflectance. Soil Sci. Amer. J. , 66 , 722 – 727 . Mahrt , L. , and M. Ek , 1984 : The influence of atmospheric stability on potential evaporation. J. Climate Appl. Meteor. , 23 , 222 – 234 . Mann , J. , and D. H. Lenschow , 1994 : Errors in airborne flux measurements. J. Geophys. Res. , 99 , 14519 – 14526 . Mitchell , K. E. , and Coauthors , 2004 : The multi-institution North American Land Data Assimilation System (NLDAS): Utilizing multiple GCIP products
) < 1; in the Kansas-experiment surface-layer data of Businger et al. (1971) , data fit the MO similarity curves out to − z / L ∼ 1.5, with a few points to 2.2. According to Wyngaard (1983) and Brutsaert (1998) , the surface layer extends to ∼10% of the PBL depth. However, the definition can be more conservative than this: Mahrt (2000) uses 5% of the convective boundary layer depth as the upper limit for the surface-layer top, and the American Meteorological Society (AMS) Glossary of
) < 1; in the Kansas-experiment surface-layer data of Businger et al. (1971) , data fit the MO similarity curves out to − z / L ∼ 1.5, with a few points to 2.2. According to Wyngaard (1983) and Brutsaert (1998) , the surface layer extends to ∼10% of the PBL depth. However, the definition can be more conservative than this: Mahrt (2000) uses 5% of the convective boundary layer depth as the upper limit for the surface-layer top, and the American Meteorological Society (AMS) Glossary of
event description Four CI events compose our dataset from which the accuracy assessments are determined (see Table 2 ). Three of these events compose the training dataset. These were within a humid subtropical environment over north Alabama and south-central Tennessee. One other event used to evaluate the analysis is for a drier convective environment over Kansas. It is understood that the IR interest fields used within the MB06 algorithm will vary somewhat across convective environments (i
event description Four CI events compose our dataset from which the accuracy assessments are determined (see Table 2 ). Three of these events compose the training dataset. These were within a humid subtropical environment over north Alabama and south-central Tennessee. One other event used to evaluate the analysis is for a drier convective environment over Kansas. It is understood that the IR interest fields used within the MB06 algorithm will vary somewhat across convective environments (i
North America. J. Climate , 9 , 1288 – 1298 . Trier , S. B. , F. Chen , and K. W. Manning , 2004 : A study of convection initiation in a mesoscale model using high-resolution land surface initial conditions. Mon. Wea. Rev. , 132 , 2954 – 2976 . Trier , S. B. , C. A. Davis , D. A. Ahijevych , M. L. Weisman , and G. H. Bryan , 2006 : Mechanisms supporting long-lived episodes of propagating nocturnal convection within a 7-day WRF model simulation. J. Atmos. Sci. , 63
North America. J. Climate , 9 , 1288 – 1298 . Trier , S. B. , F. Chen , and K. W. Manning , 2004 : A study of convection initiation in a mesoscale model using high-resolution land surface initial conditions. Mon. Wea. Rev. , 132 , 2954 – 2976 . Trier , S. B. , C. A. Davis , D. A. Ahijevych , M. L. Weisman , and G. H. Bryan , 2006 : Mechanisms supporting long-lived episodes of propagating nocturnal convection within a 7-day WRF model simulation. J. Atmos. Sci. , 63
