Center for Snow and Avalanche Studies - CSAS

CODOS 2012 Updates  >  March 28  >  McClure Pass

Location of ParkCone CODOS SnowpitCODOS Update for McClure Pass:
March 28, 2012

Summary | Snowpack | Melt Rate | Stream Flows | Forecast |
Previous Update | pdf


Colorado’s substantially sub-par reservoir of SWE now contains two significant (D5 and D4) and one minor (D6) dust layers at/near the snowpack surface statewide, and is vulnerable to continued prolonged periods of dry, sunny weather combined with reduced snow albedo.  This Update presents site-by-site and summary analyses of snowmelt rates at CODOS and other Snotel sites for Water Years 2006-2011.

Snowpack conditions in the upper Crystal River, North Fork of the Gunnison, and Muddy Creek watersheds are likely still mixed, with cold content persisting in alpine and higher sub-alpine terrain snow at the same time that lower elevation snowcover has become isothermal and begun releasing snowmelt runoff.   Merged dust layers D6/D5/D4 are reducing snow albedo throughout these watersheds. The low-elevation McClure Pass Snotel site has shown accelerating declines in SWE while the nearby higher-elevation Schofield Pass Snotel shows only a small decline during the same period.  Should dry weather continue to dominate this spring season, and dust-enhanced snowmelt rates approach the average or maximum rates discussed below, snow all gone (SAG) may occur early at these Snotel sites producing early peak streamflows, early passage of runoff center of mass, and steep descending limbs on Crystal River, North Fork of the Gunnison, and Muddy Creek hydrographs.

SnowPack Discussion

We have no new first-hand snowpack observations to present.  Our next visit to the McClure Pass site will be in early April,
as weather and dust conditions dictate.

Melt Rate

The table below presents Water Year analyses of snowmelt behavior at the Snotel station adjoining this CODOS site beginning with WY 2006.  The date of Peak SWE and subsequent number of days to “snow all gone” (SAG) are shown for each Water Year.  Then, the amount of additional SWE received after the date of Peak SWE is added to Peak SWE to calculate an “adjusted daily mean loss [of] SWE” rate during the snowmelt season that Year.  Finally, the mean air temperature during the period from Peak SWE to SAG, as measured at the Snotel site, is shown for each Water Year.  A current Snotel plot is presented below the table.  The intent of this table is to refresh memories of snowmelt rates during the past several dust-influenced Spring seasons, and to assess this year’s snowpack conditions in light of those past years.

As of Tuesday, March 27, 2012, the McClure Pass Snotel had reported a loss of 1.5” SWE since March 21, for an average of 0.2” SWE loss per day, following the small bump in SWE produced by the March 18 snowstorm that delivered D5.  This recent melt rate falls short of the mean daily loss rates shown in the table below, and very far short of the maximum SWE loss rate last Spring of 1.78” per day, over a 5-day period ending May 30, 2011.

Nearby, although we do not routinely visit the site, the higher-elevation Schofield Pass Snotel data (see snowmelt analysis table and SNOTEL graph) also depicts Crystal River watershed snowmelt behavior).  As of March 27, this Snotel also reports only a small loss of 0.3” SWE since March 21st, also well short of the mean daily loss rates shown in the table, and very far short of the maximum SWE loss rate last Spring of 2.44” per day, over a 5-day period ending June 29, 2011.

Finally, farther east at the headwater of the Roaring Fork River, the Independence Pass Snotel (see snowmelt analysis table and SNOTEL graph) reflects snowmelt behavior in that watershed.  Recent data show an accelerating decline in SWE to a level outside (below) the historic range at that site. 

  McClure Pass Snotel Melt Rate Summary Table

McClure Pagano Plot

Stream Flows

Streamflow data reflect a variety of processes influencing runoff rates, but recent data from the USGS Crystal River above Avalanche Creek near Redstone stream gauge does include the influence of the reduction of snow albedo by D4 and very warm temperatures from March 10-17, a decline flows with restoration of higher snow albedo (with cooler weather) on March 18, and then another rapid increase in flows with the subsequent warmup and reduction in snow albedo as D5 emerged and merged with D4.  Event D6 may also be contributing to the most recent data.

The Colorado Division of Water Resources’ Muddy Creek above Paonia Reservoir stream gauge shows a similar pattern, but most recent flows are declining and may indicate that the center of snowmelt (SWE) mass has already passed.

Data from the USGS North Fork of the Gunnison appear to include ice-related noise but also show increasing flows, above historic median values.

Hydrograph for Crystal River near Redstone   Hydrograph for North Fork of the Gunnison River

Hydrograph for past 30 days (Feb 26 - March 27) on Muddy Creek
Hydrograph for past month of Muddy Creek


As of Tuesday afternoon forecasters at the Grand Junction National Weather Service anticipate continued warm and generally dry weather through the remainder of this week, with the warmest temperatures of the week on Saturday. The northern mountains may experience some light showers and more cloudiness than the southern half of the state.  Snowmelt rates are likely to continue to increase through Saturday.

By Saturday afternoon an approaching trough and associated cold front are expected to generate another episode of strong pre-frontal SW’ly winds for the State.  Winds will sustain and become W’ly on Sunday.  Dust source areas in the Colorado Plateau may yield to these SW’ly and W’ly winds and produce another dust event beginning Saturday afternoon.  This weekend’s cold front may, once again, not deliver a significant winter storm.  However, a return to cooler, more seasonable temperatures by Sunday/Monday does seem likely.  In the absence of new snow with this weekend cold front, a dry D7 event, should it occur, would generally fall directly onto already exposed and merged D6/D5/D4 dust, further reducing snowpack albedo throughout the Colorado mountains.