The moisture problem stems from the fact that we haven't really had a trough take a southerly-enough track since the beginning of the month to induce deep, strong onshore flow from the Gulf, and thus the metaphorical "firehose" of moisture from the Gulf has been more like a trickle or has been shut off. The decent moisture that is in place currently is the result of 10+ days of no cold fronts to clear out the moisture + ET + what little trickle of moisture is actually coming in off the Gulf.
As long as we continue to be locked into this split-flow pattern where the main polar jet is along or north of the Canadian border and all we get are these measly cutoffs oozing into the Rockies before stalling and filling, there will be insufficient widespread flow for supercells and also generally no synoptic scale moisture return off the Gulf. Can't say return flow off the western Atlantic is out of the question, but the trajectories needed for such moisture to reach the Plains are less than probable. It also doesn't help that the subtropical jet is a bit far south and for some reason is failing to generate the troughs we would need to see good Plains setups.
I think I mentioned this before, but this kind of seasonal evolution is why I hate seeing really active troughing patterns in March-early April. I know this isn't entirely scientific to say, but it does seem like that type of pattern (frequent high-amplitude troughs crossing the CONUS) exhausts itself after a few weeks or up to a month or two, and then it seems like it has to reload. So when that pattern sets up too early, you get this death ridge/split flow/zonal flow lameass crap during the climatological peak of the season. What I like to see is the active troughing pattern set up starting mid-late April so that synoptic-scale cyclogenesis episodes coincide with the stronger diabatic heating and better moisture return of mid-late spring rather than early spring when CP air masses still pervade the eastern 2/3rds of the US and moisture is always questionable. In the former cases you're much more likely to have the ingredients in place for a prolonged period of more significant severe events, at least a few of which are bound to promote satisfying chase setups and/or tornado outbreaks.
As long as we continue to be locked into this split-flow pattern where the main polar jet is along or north of the Canadian border and all we get are these measly cutoffs oozing into the Rockies before stalling and filling, there will be insufficient widespread flow for supercells and also generally no synoptic scale moisture return off the Gulf. Can't say return flow off the western Atlantic is out of the question, but the trajectories needed for such moisture to reach the Plains are less than probable. It also doesn't help that the subtropical jet is a bit far south and for some reason is failing to generate the troughs we would need to see good Plains setups.
I think I mentioned this before, but this kind of seasonal evolution is why I hate seeing really active troughing patterns in March-early April. I know this isn't entirely scientific to say, but it does seem like that type of pattern (frequent high-amplitude troughs crossing the CONUS) exhausts itself after a few weeks or up to a month or two, and then it seems like it has to reload. So when that pattern sets up too early, you get this death ridge/split flow/zonal flow lameass crap during the climatological peak of the season. What I like to see is the active troughing pattern set up starting mid-late April so that synoptic-scale cyclogenesis episodes coincide with the stronger diabatic heating and better moisture return of mid-late spring rather than early spring when CP air masses still pervade the eastern 2/3rds of the US and moisture is always questionable. In the former cases you're much more likely to have the ingredients in place for a prolonged period of more significant severe events, at least a few of which are bound to promote satisfying chase setups and/or tornado outbreaks.