Preparing for the 2015-16 OLYMPEX Field Campaign: Challenges of observing heavy rain and snow in remote regions of the Olympic Mountains Joe Zagrodnik.

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Presentation transcript:

Preparing for the 2015-16 OLYMPEX Field Campaign: Challenges of observing heavy rain and snow in remote regions of the Olympic Mountains Joe Zagrodnik Lynn McMurdie, Robert Houze University of Washington Pacific NW Weather Workshop Feb 27, 2015

Olympic Mountains site… Ideal ground site… Olympic Mountains site… To start, I'll give a little overview of what goes into creating the network of ground sites. Envision the ideal ground site like this one from a prior NASA campain in Iowa. A nice wide open field--perhaps too wide open, but plenty of room and no obstructions Then there are the Olympic Mountains. This is an actual site and there is a person in there--we had a rain gauge there but the site is becoming overgrown.

Ground Site Criteria Science objectives Permission Accessibility National Park Service Quinault Indian Nation National Forest Service Fish and Wildlife Service NOAA WS DOT Local Government Private Landowners Accessibility Communication Electricity Vegetation Security To meet the science objectives that Lynn discussed, the sites should follow the progression of precipitation as it is modified/enhanced by topography. However, there are a number of other factors that have to be considered. First, you need permission from the land/site owner, which is the National Park Service, Forest Service, Quinault Indian Nation, Fish&Wildlife Service, NOAA, WS DOT, Communications companies, local government, and private landowners. Then there is accessibility—there are not many roads in the study area, some are dirt roads that have experienced mudslides, blowdowns, and snow blocking the road, while the Upper Quinault/Enchated Valley site requires 13 miles of hiking to reach the instruments. Communication—cell phone tower connection is preferred, otherwise sites have to be frequently inspected to ensure they are operating Electricity is only available at about half of our sites, the other half are powered by solar and battery power—but of course there are a lot of clouds and trees in our state so there are challenges associated with that. Vegetation—rain measurements are not accurate if vegetation is too close, but an exposed, open site is not ideal Security—don’t want the instruments to be stolen, but fortunately there isn’t too much of a market for plastic rain buckets. However, rain gauges do not function with bullet holes in them—and they also don’t work when Elk or bears tip them over.

Ground Site Locations So the planning decisions have resulted in a network of 12 sites, about half of which have power, and most of which are accessible by road, except the site well up the Quinault Valley which would be highly beneficial

Snoqualmie Pass Trailer Test Simulating high altitude, no power conditions Deployed Nov 4, 2014

Questions to answer How long can the batteries last? Can instruments operate on batteries without heating element? Do the instruments make accurate and useful microphysical measurements? How often is maintenance needed?

Q: How long can the battery last? (Set of 8 deep-cycle batteries + 140 W solar panel) Sunny periods Point out downward trend…trailer is in favorable location, Olympics are more cloudy A: About one month if no sun, all winter if there are sunny periods

Q: Can instruments operate on batteries without heating element? Parsivel disdrometer Pluvio bucket

Accumulated Precipitation NW Avalanche Center: 50.55 mm Chunk of snow drops in bucket Red: Pluvio (bucket) Blue: Parsivel (disdrometer)

Q: Can instruments operate on batteries without heating element? A: Usually* *Currently having issues with condensation inside of Parsivel head. Attempting to use silica gel desiccant packets to remove moisture. Preliminary results are encouraging.

Do the instruments make accurate and useful microphysical measurements? Case Study: Jan 18, 2015

Frontal cyclone crossing a mountain range Prefrontal Observed as frontal sector crosses topography The general picture fits well with previous studies. As a frontal cyclone approaches topography, the structure of the precipitation changes in different regions of the system, and is modified by the terrain Medina et al (2007) studied radar observations over the Oregon Cascades -Early sector: warm front/warm advection, leading edge echo appears aloft and descends to surface, light/uniform precip -Middle sector: low/cold/occluded front, besides the bright band (melting layer), a second, higher enhanced layer has been observed. Forced by vertically propagating gravity waves or growth by aggregation? Turbulent layer enhances hydrometer growth -Late sector: Broadened by orographic lift as small, shallow convective cells approach topography -We are especially interested in the variations in the brightband height and the microphysics because we are better equipped to study these features compared with previous field studies Postfrontal precipitation broadened by orographic uplift Medina et al. (2007)

IR Satellite Jan 18, 2015 Prefrontal: Jan 18 00 UTC Typical storm from this winter—coming from the southwest, high moisture content, mostly liquid

KATX Radar Prefrontal: stratiform precipitation Frontal: Increase in intensity Postfrontal: shallow, convective showers

Reflectivity and Precip Accumulation Prefrontal Frontal Postfrontal In this event, the precip was nearly all rain. There was only occasional mixing of sleet and snow. The Parsivel data shows relatively smooth reflectivity averaging 25-35 dBZ during the prefrontal period. In this case, we did not observe significant frontal enhancement. The postfrontal period is clearly marked by a greater variation in reflectivity—but almost no breaks in the precipitation. Precip accumulated 75 mm (3 inches) during this 24-hr period. We’ve observed

Particle Size Distribution Prefrontal Frontal Postfrontal

Q: How often is maintenance needed? Q: Can Instruments make accurate and useful microphysical measurements? A: Yes! Q: How often is maintenance needed? A: Every 3 weeks or so

Thank you! Follow us on Twitter @UW_OLYMPEX Trailer test data is available at the following URL (or email jzagrod@uw.edu for link): http://www.atmos.washington.edu/~jzagrod/olympex/apu31/ Today at Snoqualmie Pass (through 10 AM):

Extra Slides

Management Needs Type # Sites Visit Frequency Data Retrieval Access Issues Low elevation with power 4 4-6 weeks, as needed Cell - Low elevation, no power 1-2 weeks, as needed Site dependent Mudslides High elevation with Power* 2 Snow, road closures High Elevation, no power ? No vehicle access *As needed is very important—after a major 10-15” rainstorm, all Pluvios will have to be emptied *It is expected that snow/rime removal and heavier precip rates will require higher elevation sites to be visited more frequently *Includes Hurricane Ridge

Accessibility US-101 Maintained Dirt Road Paved Road Mudslides likely 13-mile backcountry trail Unmaintained after Oct-1 Snow, mudslides possible US-101 Maintained Dirt Road Paved Road Unmaintained Dirt Road