Case Description: 5 December 2018

Summary

Three cells initiate and grow near the AMF into small sizes

Description

Convection early during the day clears out of the region by 10 UTC and convective initiations start by 17 UTC. By 19:45 UTC, three cells develop and grow to the north of the AMF and one to the southwest behind the ridgeline (not observable by the CSAPR2). CAPE values are in the lower third of their ranges (at 18 UTC MUCAPE=823; MLCAPE=519 J kg-1).

Available assets

CSAPR2, G1 flight, GOES rapid scan, RELAMPAGO mission (35 soundings), CSU C-Band data

Critical period: 17:00–20:00

17:00 System initiates over AMF and grows
17:45 Second system initiates north of the AMF and grows
18:45 Third system initiates north of the AMF and grows
19:45 Fourth system initiates to the SW of the AMF behind the ridgeline
Brightness temperature, 2018-12-05 19:45 UTC

Figure 5 GOES16 band 13 brightness temperature at 2018-12-05 at 19:45 UTC. Three systems initiate northeast of the AMF and one to the southwest.

Available LES ensemble members

Table 5 Summary of LES cloud behavior for 2018-12-05

Impression

Ensemble Member

Cloud Behavior

Bust

EDA05-Morr

Really overdoes it.

Bust

ERA5-Morr

At observed convective initiation, the simulation already has a ver large convective system over the AMF.

Dud

GEFS01

Initiates to northwest on ridge versus observations and 0.5 h late. Systems are seriously underdeveloped.

Dud

GEFS01-Smag

SGS sensitivity test with Smagorinksy using default parameters. Similar behavior to GEFS01.

Dud

GEFS01-SmagCs

SGS sensitivity test with Smagorinsky and modified Cs parameter. Similar behavior to GEFS01.

Dud

GEFS01-TKECk

SGS sensitivity test with TKE an modified Ck parameter. Similar behavior to GEFS01.

Poor

GEFS01-Morr

Initiates northwest 0.5 h late. Development is blobular versus observation’s line and misses norther cell. By 19 UTC, looks similar to observations, though lacks the northeast cell at perimeter.

Bad

GEFS02-Morr

Scattered convection before observed convective onset, which then broaden further. The ‘hits’ for skill scoring tend to arise from broad convection that happened to overlap the observations despite the simulated structure being very different from what occurred.