Given the latest Sedalia dewpoint of 55, I'm inclined to give the cooperative sites you cited more credence. Now the question is, how did this moist blob get there? It's almost as though a little bubble of moister air somehow formed north of or broke off from the main blob farther south. Perhaps there is moister air just above the surface associated with the nocturnal LLJ, and the vigorous convection locally mixed it down to the surface?
...
Given that Sedalia (actually, the site is at Whiteman AFB) is now back down to a dewpoint of 52, and given the progression of observations SZL reported, I'm inclined to think that the observations, at least at SZL, were related to the storm modifying its surface environment:
KSZL 010255Z 16008KT 10SM BKN160 17/11 A2937 RMK AO2A PRESFR SLP948 58010=
KSZL 010312Z 15010KT 7SM -SHRA OVC160 17/12 A2936 RMK CONS LTG ICCCCG DSNT SW TS 20SW MOV NE=
KSZL 010324Z 15006KT 7SM -TSRA BKN050CB OVC160 17/12 A2936 RMK CONS LTG ICCCCG OHD TS OHD MOV NE=
KSZL 010340Z 14005G15KT 7SM -TSRAGR BKN050CB OVC160 17/12 A2936 RMK CONS LTG ICCCCG OHD TS OHD MOV NE GR 1/2=
KSZL 010347Z 14005G15KT 1 1/2SM TSRA BKN030CB OVC160 16/12 A2936 RMK CONS LTG ICCCCG OHD TS OHD MOV NE=
KSZL 010347Z 14005G15KT 1SM TSRAGR BKN030CB OVC160 16/12 A2936 RMK CONS LTG ICCCCG OHD TS OHD MOV NE GR 1/2=
KSZL 010353Z 09009KT 3/4SM +TSRAGR BKN020CB OVC160 15/12 A2936 RMK CONS LTG ICCCCG OHD TS OHD MOV NE GR 1/2=
KSZL 010355Z 16007G15KT 3/4SM +TSRAGR OVC030CB 16/13 A2937 RMK AO2A CONS LTG ICCCCG OHD TS OHD MOV NE GR 3/4 SLP944=
KSZL 010356Z 14011G15KT 3/4SM R01/2000VP6000FT TS +RA BKN019 15/12 A2937 RMK AO2A VIS 2 RWY19 LTG DSNT N - S AND W CIG 012
RWY19 SLP944=
KSZL 010412Z 36004G29KT 2SM -TSRA FEW001 BKN020CB OVC160 14/13 A2935 RMK CONS LTG ICCCCG OHD TS OHD MOV NE=
KSZL 010440Z 12007KT 10SM TS BKN030CB OVC100 15/13 A2930 RMK CONS LTG ICCCCG OHD TS OHD MOV NE=
KSZL 010455Z 16015G19KT 10SM TS OVC037 15/12 A2928 RMK AO2A PK WND 24029/0403 CON LTG OHD TS OHD MOV NE PRESFR SLP914=
KSZL 010505Z 31013G25KT 10SM TS BKN035CB OVC100 14/11 A2935 RMK CONS LTG ICCCCG OHD TS OHD MOV NE=
What we see here is that the winds backed around to the SE and the dewpoint rose (as Paul mentioned earlier for points farther west) under the forward flank of the storm. Then as the meso passed by, the winds shifted to the north, and after a little while back around to the SSE as the dewpoint started to fall again (at the very end the next cell starts to impact their observations). This is of course consistent with the passage of a mesocyclone, except that having the dewpoint rise as the precip core passes overhead is not your typical situation. One explanation I can come up with is that there is moister air above the surface which the storm is tapping, and this is being mixed down through a very shallow layer of drier air. Or perhaps evaporational cooling is bumping up the dewpoint a bit, and the temperature down a bit. Or maybe something else entirely is going on, or was going on further west earlier.
Thoughts?