Alert archive / New Mexico / Mesoscale Discussions in 2021
Mesoscale Discussion 1062
The Storm Prediction Center issued this mesoscale discussion at Jun 22, 2021, 1:40 PM MDT for Las Animas County, Colorado; 5 counties in New Mexico. It was in force for 2 hr.
The area
The outline as issued.
The facts
- Issued
- Jun 22, 2021, 1:40 PM MDT (19:40 UTC)
- Expired
- Jun 22, 2021, 3:45 PM MDT
- In force
- 2 hr
- Issued by
- the Storm Prediction Center
- Concerning
- Severe potential...watch unlikely
- Chance of a watch
- 5%
Counties Las Animas County, CO, Colfax County, NM, Harding County, NM, Mora County, NM, San Miguel County, NM, Union County, NM
The nearest sounding before it
Amarillo Airport, TX (KAMA), launched 12:00Z, 7.7 hours before the alert went out and 281 km from the middle of its area. This is the routine balloon launch nearest before it, the air the forecaster had in hand, not a measurement taken for the alert.
- Mixed-layer CAPE
- 0 J/kg
- Mixed-layer CIN
- No buoyant parcel
- Mixed-layer LCL
- 1455 m above ground
- 0-6 km bulk shear
- 31 kt
- 0-1 km storm-relative helicity
- 5 m²/s²
- 0-3 km storm-relative helicity
- 88 m²/s²
- Significant tornado parameter
- 0.0
- Supercell composite
- 0.0
The text
As transmitted.
076
ACUS11 KWNS 221940
SWOMCD
SPC MCD 221940
COZ000-NMZ000-222145-
Mesoscale Discussion 1062
NWS Storm Prediction Center Norman OK
0240 PM CDT Tue Jun 22 2021
Areas affected...Northeast NM...Southeast CO
Concerning...Severe potential...Watch unlikely
Valid 221940Z - 222145Z
Probability of Watch Issuance...5 percent
SUMMARY...Isolated strong wind gusts are possible for the remainder
of the afternoon.
DISCUSSION...Visible satellite imagery shows deep cumulus along and
in the lee of the Sangre De Cristo Mountains in northeast NM and far
southeast CO. Overall buoyancy is low, with this deepening cumulus
primarily a result of orographic effects and modest mid-level
moisture beneath the upper ridge. The best moisture advection will
be displaced east of the region, but some additional air mass
destabilization is possible as a result of strong diurnal heating
and resulting deep boundary-layer mixing. This destabilization may
allow updrafts to persist off the higher terrain for a bit longer
from now through the remainder of the afternoon. Once these storms
do decay, evaporatively cooled downdrafts and the resulting negative
buoyancy could produce a few strong gusts at the surface, much like
what recently occurred at KLVS, producing a 61 kt gust.
..Mosier/Hart.. 06/22/2021
...Please see www.spc.noaa.gov for graphic product...
ATTN...WFO...PUB...ABQ...
LAT...LON 36910517 37590479 37910439 37990404 37830361 37660338
37410325 37180319 37010318 36360340 35680376 35240434
35090479 35230545 35640562 36910517Nearby
Mesoscale Discussions in New Mexico, 2021Mesoscale Discussions in Colorado, 2021Every mesoscale discussion in 2021
Sources
The product and its follow-ups from the Iowa Environmental Mesonet's archive of National Weather Service and Storm Prediction Center text; the sounding from the Mesonet's radiosonde archive.