NDCMP Weather Forecast

District 1District 2
Transition (UTC)01100
FirstSecondThirdFirstSecondThird
Forecasted WeatherNO SIGNO SIGNO SIG

Forecaster: Daniel Brothers

Synopsis


The upper level trough that dragged through yesterday is replaced by a small upper level ridge today. Surface dew points also remain low in D1. The combination of low moisture, no appreciable instability, and general subsidence means it will be a quiet day in Bowman. Moving into tomorrow may be different. A notable upper level low/trough moves across southern Canada tomorrow. The first push of energy rotates around this low and through D1 in the morning. There is a return of better moisture throughout the column, but at that time of day instability is still minimal. Expect some mid-level clouds to move through, but be diminshing with time as the atmosphere transitions from nocturnal mid-level forcing to a more surface based regime with day-time heating. By around briefing, or shortly after, the main surface trough and associated mid-level vorticity moves through ND. Surface dew points rebound to the upper 40s and some instability builds in the district. Cold 500mb air will also aid in developing instability and the threat for small hail. However, models are suggesting D1 may be just a bit too far south for the better forcing. 700mb vertical velocities back this up, and the passage of the trough in the early afternoon instead of a couple hours later also limits confidence in thunderstorms in the district. The HRRR keeps development just outside, but the NAM Nest does have a few storms develop in the early afternoon. It will be interesting to see what the forecast decides tomorrow.

6/6/25


Flash Flood Guidance (Click Image for 1hr, 3hr, & 6hr Graphics)

An Upper Level ridge is moving over ND today, as expected

Surface Dewpoints continue to be low today.

BPP 22Z MLCAPE showing a subsidence inversion and lack of instability

Tomorrow a notable jet streak under an upper level low/trough moves into ND

Tomorrow, the upper level low moves across southern Canada, bringing a surface trough through ND

In the mnorning, the first wave of vorticity sweeps through Bowman

Bowman sounding for tomorrow morning, more moisture returns.

NAM Nest does produce some light reflectivity in the morning, but expect this to be in the form of diminishing mid-level clouds

By near briefing the main surface trough moves through Bowman, providing forcing

Surface Dew points rebound adequately tomorrow afternoon to help with convection

By briefing, Surface Based CAPE is sufficient to support thunderstorms

Bowman sounding tomorrow at 20Z, probably the best chance for operations this weekend

tomorrow afternoon a pocket of very cold 500mb air around the upper level low is over W ND

A strong push of vorticity moves through tomorrow afternoon, but the forcing with it i less impressive in Bowman

The 700mb vertical velocity backs up the idea that forcing won't be as great in D1

HRRR reflectivity gets some convection close to the edge of D1

The NAM Nest has convection a little farther SW, which is enough to get a few storms in the district


Indices


Lifted Index
(<1)
K index
(>30)
Total Totals
(>48)
Sweat
(>200)
Cape
(>125)
CIN
(>-100)
Bulk Richarson Number
(>3)
Helicity
(>125)
D1 2.4 31.4 47.3 70 0 0 0 92
ISN 0 0 0 0 0 0 0 0
MOT 0 0 0 0 0 0 0 0

Jefferson Index
(>28.5)
Cross Totals
(>18.65)
Thompson Index
(>28.5)
S Index
(>35.8)
Showalter Index
(<=0.5)
Cap Strength
(0-2.65°C)
D1 30 17.5 29 45.3 2.2 0
ISN 0 0 0 0 0 0
MOT 0 0 0 0 0 0

Weather Features

  • Subsidence
  • Upper Level Ridge