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# Description
Not making use of the ensemble spread requires adding a few bells and
whistles to the parametric **B**. This PR allows better control of the
variance partitioning in shallow places, scaling e-fold to the local
depth.
_Draft PR until NOAA-EMC/global-workflow#3238 is
merged_
# Companion PRs
- NOAA-EMC/jcb-gdas#73
# Issues
- fixes#1491
# Automated CI tests to run in Global Workflow
<!-- Which Global Workflow CI tests are required to adequately test this
PR? -->
- [ ] atm_jjob <!-- JEDI atm single cycle DA !-->
- [ ] C96C48_ufs_hybatmDA <!-- JEDI atm cycled DA !-->
- [ ] C96C48_hybatmaerosnowDA <!-- JEDI aero/snow cycled DA !-->
- [ ] C48mx500_3DVarAOWCDA <!-- JEDI low-res marine 3DVar cycled DA !-->
- [ ] C48mx500_hybAOWCDA <!-- JEDI marine hybrid envar cycled DA !-->
- [ ] C96C48_hybatmDA <!-- GSI atm cycled DA !-->
The grid imprinting shows in the increments and there is no quick fix on the way. Remove the ensemble B as a temporary fix for now.
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