Wind and Sagebrush

Wind and Sagebrush

Wind and Sagebrush: Mountain big sagebrush (Artemisia tridentata subsp. Vaseyana) in flower - Photo Courtesy and Copyright Dr. Leila Shultz
Mountain big sagebrush (Artemisia tridentata subsp. Vaseyana) in flower – Photo Courtesy and Copyright Dr. Leila Shultz

Wind and Sagebrush:Three-tip sage (Artemisia tripartite) with visible yellow flowers. - Photo Courtesy and Copyright Dr. Leila ShultzThree-tip sage (Artemisia tripartite) with visible yellow flowers. – Photo Courtesy and Copyright Dr. Leila Shultz

Hi, I’m Holly Strand of the Quinney College of Natural Resources at Utah State University.

By late summer, most of Utah’s flowering plants have fizzled out for the year—those that remain are looking pretty spent. But not true for the sagebrush. It’s show time for over 20 types of sagebrush of the Intermountain West.

Like grasses and conifers, sagebrush plants are pollinated by the wind. They have no need for the specialized traits designed to attract live pollinators. Instead, they have evolved other strategies to survive and multiply.

For instance, wind-pollinated plants don’t need showy, colorful petals to attract insects or birds. The wind is going to do its job anyway regardless of visual cues. Thus sagebrush flowers are very small and nondescript. In fact, when passing by flowering sagebrush you might not even notice that it’s in bloom. Look for long spikes with clusters of tiny flower heads. The pale yellow flowers are concealed by petal-like bracts, which are the very same color as the rest of the plant.

While the flowers of sagebrush lack in beauty, they make up in quantity. A single flowering stem of the most common sagebrush—known simply as big sagebrush–can hold hundreds of flower heads that produce a massive amount of pollen. Most wind-blown pollen grains won’t end up anywhere near the female part of another plant. So to make up for this risky method of fertilization, individual plants must produce greater volumes of pollen. In contrast, plants with live pollinators get door to door service during fertilization. Far less pollen is needed to get the same job done.

Scent is another way for plants to attract live pollinators. Species pollinated by bees and flies have sweet scents, whereas those pollinated by beetles have strong musty, spicy, or fruity odors. However, the iconic western scent of the sagebrush has absolutely nothing to do with pollination. Instead, the pungent aroma of the sagebrush is a by-product of certain chemicals produced in the leaves. These chemicals evolved to repel animals and to reduce the odds of being eaten or grazed.

The chemicals—bitter terpenes, camphors and other secondary compounds–—peak in early spring. But as the late-summer flowering period approaches, the chemicals start to break down. By winter, browsers like deer and elk can nibble on the protein-rich seed heads without getting a nasty aftertaste.

Thanks to botanist Leila Shultz for sharing her knowledge of sagebrush. For a link to the online version of Leila’s book Pocket Guide to Sagebrush, go to www.wildaboututah.org
If you’d like a hard copy of this Pocket Guide, send an email to wildaboututah@gmail.com We have 5 copies to give away to listeners from across the state.

For Wild About Utah and the Quinney College of Natural Resources, I’m Holly Strand.

NOTE: The copies are gone. You can view the book as a .pdf here or check here for the next printing from https://www.sagestep.org/pubs/brushguide.html.

Credits:

Photo Courtesy & Copyright 2007 Dr. Leila Shultz
Text: Holly Strand, Quinney College of Natural Resources at Utah State University

Additional Reading:

Dudareva, Natalia. 2005. Why do flowers have scents? Scientific American April 18. https://www.scientificamerican.com/article/why-do-flowers-have-scent/

Shultz, Leila. 2012. Pocket Guide to Sagebrush. PRBO Conservation Science. https://digitalcommons.usu.edu/sagestep_reports/20/
As pdf: https://rdjzr2agvvkijm6n3b66365n-wpengine.netdna-ssl.com/wp-content/uploads/2018/06/sagebrush_pock_guide_reduced.pdf

Shultz, L. M. 2006. The Genus Artemisia (Asteraceae: Anthemideae). In The Flora of North America north of Mexico, vol. 19: Asterales, pp. 503–534. Flora of North America Editorial Committee, eds. Oxford University Press. New York and Oxford.

USDA, NRCS. 2012. The PLANTS Database, National Plant Data Team, United States Department of Agriculture (USDA), Natural Resource Conservation Service (NRCS): https://www.plants.usda.gov

VanBuren, R., J. C. Cooper, L. M. Shultz and K. T. Harper. 2011. Woody Plants of Utah. Utah State University Press & Univ. Colorado. 513 pp. https://upcolorado.com/utah-state-university-press/woody-plants-of-utah

Dust in the Wind

Dust Storm Milford Flats
4 March 2009
US Geological Survey photo by Mark Miller


Hi, I’m Holly Strand of the Quinney College of Natural Resources at Utah State University.

American paleontologist Roy Chapman Andrews was a frequent visitor to the Gobi Desert. This is how he described being caught in a Gobi desert dust storm: “Seemingly a raging devil stood beside my head with buckets of sand, ready to dash them into my face…” “…after each raging attack it would draw off for a few moments’ rest. Then suddenly the storm devil was on us again, clawing, striking, ripping, seeming to roar in fury that any of the tents still stood.”

Andrews didn’t have to go so far to feel the rage of a dust storm. He could have come to western Utah. While we don’t have the monstrous storms of the Sahara and the Gobi/Manchurian deserts, the eastern Great Basin–which is essentially western Utah–sits secure on any global list of dust storm hotspots.

Let’s consider why this is so…

First and foremost, western Utah has the dust. In scientific terms, dust is any particle—organic or inorganic—that is less than .63 microns or smaller in diameter. .63 microns is about half the width of a single human hair. In geological terms think silt or clay particles. A grain of sand is much larger. If you are the size of a dust particle, then a relatively small puff of wind will release you into the air. And you’ll stay there until it’s completely calm or rain forces you down.

A great place to find geologic dust is in desert playas. For runoff sediments collect in these dry lake depressions. Western Utah has several of these desert dust bins. And satellite data have confirmed that playas such as Sevier Dry Lake, Tule Dry Lake, and Great Salt Lake Desert are major sources of dust plumes. The alluvial fans of the Great Basin mountains provide an additional source of dust.

To get this dust airborne you need wind which is also plentiful in western Utah. This region typically experiences strong south and southerwesterly winds called “hatu winds.” That’s Utah spelled backwards. The name was coined by colorful Utah meteorologist Mark Eubank. These hatu winds blow south to north or to the northwest. They pick up speed and dust as they race along the north-south trending Great Basin ridges. They can reach speeds of over 90 miles per hour.

Utah’s hatu winds peak in the spring months with a secondary peak in August-September. In spring these windy freight trains full of dust can hit the populated Wasatch Front wreaking havoc with air quality and human health.

Sometimes raindrops capture dust in the airstream and splat them onto our windshields and windows. These mud rains are most common in spring when the hatus are at their peak. And this is why saavy Utahns never bother washing their home windows until June.

While dust storms can be considered natural events, the fact that they are increasing in number and severity is definitely unnatural. The increase is caused by human-related activities that remove vegetation or break the biological soil crusts that help stabilize dust and soil. Overgrazing, water withdrawals, military operations, farming on marginal lands, off-road vehicle riding, fires, even restoration activities all release dust to be carried off by the next significant wind.

Thanks to Atmospheric Scientist Maura Hahnenberger for her help with this Wild About Utah story.

For Wild About Utah, and the Quinney College of Natural Resources, I’m Holly Strand.

Credits:

Images: Courtesy USGS.gov and NRCS.gov
Theme: Courtesy & Copyright Don Anderson as performed by Leaping Lulu
Sound: Wind sound effect from Sound Bible.com Recorded by Mark DiAngelo https://soundbible.com/1810-Wind.html
Text: Holly Strand

Sources & Additional Reading

Hahnenberger, M. and K. Nicoll. Geomorphic and land use characteristics of dust sources in the eastern Great Basin of Utah, U.S.A. Accepted Geomorphology. https://georesearch.ir/article-1-381-en.html

Hahnenberger, M. and K. Nicoll, 2012. Meteorological characteristics of dust storm events in the eastern Great Basin of Utah, U.S.A. Atmospheric Environment, 60, 601-612. https://doi.org/10.1016/j.atmosenv.2012.06.029, https://www.sciencedirect.com/science/article/abs/pii/S1352231012005808?via%3Dihub
https://sci-hub.se/https://doi.org/10.1016/j.atmosenv.2012.06.029

Jason P Field, Jayne Belnap, David D Breshears, Jason C Neff, Gregory S Okin, Jeffrey J Whicker, Thomas H Painter, Sujith Ravi, Marith C Reheis, and Richard L Reynolds The ecology of dust Front Ecol Environ 2010; 8(8): 423–430, doi:10.1890/090050 (published online 12 Oct 2009)https://www.esajournals.org/doi/pdf/10.1890/090050
https://sci-hub.se/https://www.esajournals.org/doi/pdf/10.1890/090050

Neff, J. C., A. P. Ballantyne, G. L. Farmer, N. M. Mahowald, J. L. Conroy, C. C. Landry, J. T. Overpeck, T. H. Painter, C. R. Lawrence, and R. L. Reynolds, 2008: Increasing eolian dust deposition in the western United States linked to human activity. Nature, 1, 189-195
https://www.nature.com/articles/ngeo133
https://sci-hub.se/https://doi.org/10.1038/ngeo133

Warner, Thomas T. 2004. Desert Meteorology. NY: Cambridge University Press
https://www.cambridge.org/core/books/desert-meteorology/830636E147078337D24957845F6A6855
https://doi.org/10.1256/wea.201.04

Washington, R., M. Todd, N. J. Middleton and A. S. Goudie, 2003. Dust-storm source areas determined by the Total Ozone Mapping Spectrometer and Surface Observations, Annals of the Association of American Geographers, 93(2), 297-313.
https://onlinelibrary.wiley.com/doi/abs/10.1111/1467-8306.9302003
https://sci-hub.se/https://doi.org/10.1111/1467-8306.9302003

Miller, M. E., et al. (2012). “Post-fire land treatments and wind erosion – Lessons from the Milford Flat Fire, UT, USA.” Aeolian Research 7: 29-44.
https://www.sciencedirect.com/science/article/abs/pii/S1875963712000171
https://sci-hub.se/https://doi.org/10.1016/j.aeolia.2012.04.001

Steenburgh, W. J., et al. (2012). “Episodic Dust Events of Utah’s Wasatch Front and Adjoining Region.” Journal of Applied Meteorology and Climatology 51(9): 1654-1669.
https://journals.ametsoc.org/view/journals/apme/51/9/jamc-d-12-07.1.xml

Cloud classification

Cloud classification: Wispy high-flying cirrus clouds made of ice crystals. Courtesy & © Jim Cane, Photographer
Wispy high-flying cirrus clouds
made of ice crystals.

Courtesy & © Jim Cane, Photographer
 
Cloud classification: A dark monotonous low deck of stratus clouds. Courtesy and Copyright Jim Cane, PhotographerA dark monotonous low deck
of stratus clouds.
Courtesy & © Jim Cane, Photographer
 
Cloud classification: Fair-weather cumulus clouds with flat bottoms and puffy tops.Fair-weather cumulus clouds
with flat bottoms and puffy tops.
Courtesy & © Jim Cane, Photographer
 
Fair-weather cumulus clouds with flat bottoms and puffy tops.Fair-weather cumulus clouds
with flat bottoms and puffy tops.
Courtesy & © Jim Cane, Photographer

 
A dense cloud that grows upward, looks like a cauliflower, anvil, or tower, and usually has lightning, thunder, and rain.Cumulonimbus
A dense cloud that grows upward, looks like a cauliflower, anvil, or tower, and usually has lightning, thunder, and rain.
Courtesy NOAA


Who has not indulged in the idle pastime of watching puffy white clouds pass overhead, naming their shapes as they form? Of course, such whimsical names do not serve comparative description and understanding. For this, a lexicon of clouds is needed. Our formal cloud classification system traces back to 1803, when an Englishman, Luke Howard, published “An essay on the modifications of clouds”. Luke Howard owned a profitable pharmaceutical company, which funded his gentlemanly meteorological pursuits. Mr. Howard wisely chose a Latin cloud vocabulary to name and illustrate three fundamental cloud types.

The highest flying clouds he named cirrus, meaning curl or tuft, as of hair. These wispy clouds often resemble fibers; one form is the aptly named horse-tail cirrus. Composed of ice crystals, cirrus clouds form at around 30,000 feet, about the cruising altitude of passenger jets. Wispy cirrus clouds often portend a stormy Pacific low-pressure system en route to Utah.

Howard dubbed a type of lower elevation cloud cumulus, meaning mass or heap. These grow from mere puffs to big flat-bottomed clouds with white cauliflower tops. For sheer meteorological beauty, nothing beats legions of fair weather cumulus scudding across a bluebird sky atop a montane backdrop.

The lowest cloud form is stratus. Forming below 8000 feet, they appear as an extensive deck of unbroken gray. Stratus clouds often bring Utah’s winter snowstorms and spring rains. Nimbostratus are responsible for Seattle and Portland’s endless winter drizzle. In contrast, our Utah summer rains fall from towering cumulonimbus thunder heads. These ominous clouds are powered by hot summer updrafts and the steamy humidity that flows northward with the North American monsoon.

Luke Howard’s cloud-naming convention includes 10 principal types in all which easily lend themselves to naming combinations. You can now envision the height and appearance of cirrocumulus clouds, for instance. Cirrus, cumulus, stratus, nimbus, the cloud lexicon of amateur meteorologist Luke Howard has endured for over 200 years. Pictures of these cloud types with a link to the pages of Howard’s original published treatise can be found at our Wild About Utah website.

This is Linda Kervin for Bridgerland Audubon Society.

Credits:
Images: Courtesy NOAA and
             Courtesy & Copyright Jim Cane
Text: Jim Cane, Bridgerland Audubon SocietyBridgerland Audubon Society, https://bridgerlandaudubon.org/
Voice: Linda Kervin, Bridgerland Audubon SocietyBridgerland Audubon Society, https://bridgerlandaudubon.org/

Additional Reading:

Luke Howard. 1803. “Essay on the modifications of clouds by “3rd ed. Published 1865 by John Churchill & Sons in London .
https://archive.org/details/essayonmodifica00howagoog and
https://books.google.com/books?id=7BbPAAAAMAAJ&printsec=frontcover#v=onepage&q&f=false

Riehl, Herbert. 1978. “Introduction to the Atmosphere.” McGraw-Hill, NY.
https://www.amazon.com/Introduction-Atmosphere-Herbert-Riehl/dp/0070526567

International Cloud Atlas, World Meteorological Organization,https://cloudatlas.wmo.int/home.html

Those Howling East Winds

Those Howling East Winds: Normal Diurnal Wind Shift Along the Wasatch Front, Courtesy Utah Division of Air Quality
Normal Diurnal Wind Shift
Along the Wasatch Front
Courtesy Utah Division of Air Quality

Those Howling East Winds: Air Pressure at the Surface, A Bit of a Blow..., Utah Climate Notes, January 2012, Courtesy Utah Climate Center, Utah State University Air Pressure at the Surface, 1 Dec 2011
Blue=Low Pressure, Red=High Pressure
The spacing of the lines is a measure of the pressure gradient: the closer the lines, the higher the pressure gradient. https://climate.usurf.usu.edu/news/010512Utah%20Climate%20Update%20(Jan%2012).pdf[Feb 6, 2014]
Read: A Bit of a Blow…
Courtesy Utah Climate Center, Utah State University

Wind is inevitable on a spinning planet with an atmosphere and a sun. At our latitude, westerlies prevail, but east winds do occur now and then. Locally, canyons daily exhale denser, cooler mountain air that drains into valleys. In Logan, trees blown by these canyon winds tilt westward. Occasionally, though, the whole Wasatch front is whipped by howling gales from the east, leaving behind shredded shingles, snapped tree limbs and rolled tractor-trailers. These forceful east wind events have a regional weather origin that is intensified by local topography.

It begins with a strong high-pressure cell parked over southwestern Wyoming.  It’s descending dry air circulates clockwise. Somewhere to the south or southwest, a low-pressure cell is needed.  The strong air pressure gradient between high and low generates a wind that races westward from Wyoming. The surging wind pours over the entire Wasatch front like water over a flat boulder in rapids.  These winds then plunge down slope, blowing quickest where the descent is long, steep, and unobstructed. The down rushing air slams onto the flat benches and valley floors.  In November 2011, such winds ripped Centerville with 100 MPH gusts.

Where these so-called mountain wave events blow regularly they often have names.  The mistral and foehn winds howl down from the Alps, chinooks  race down the Rocky Mountain Front Range, and the Santa Anas blast Southern California. The steep altitudinal descent of these parched winds compressively heats the air. A spark or flame soon transforms to a raging wildfire when fanned by a drying foehn or Santa Ana wind.  Europe’s foehns are also known to spark short tempers and stress.

Perhaps the sporadic easterly gales that lash the Wasatch Front and Cache Valley deserve an evocative name too.  For now, you at least know the answer to what’s blowin’ in the east wind.

Thanks to Martin Schroeder at the Utah Climate Center for insights and the stream boulder analogy

This is Linda Kervin for Bridgerland Audubon Society.

Credits:
Diurnal Utah Winds Image: Courtesy Utah Division of Air Quality
Surface Air Pressure 1 Dec 2011 Image: Courtesy Utah Climate Center, USU
Text: Jim Cane

Additional Reading:

Martin Price, Alton Byers, Donald Friend, Thomas Kohler, Larry W. Price. 2013. Mountain Geography: Physical and Human Dimensions. Univ of California Press. pages 71­74. https://www.amazon.com/Mountain-Geography-Physical-Human-Dimensions/dp/0520254317

Mesmerizing live wind map of US at:  https://hint.fm/wind/

Forecast of damaging east winds along the Wasatch Front, end of November 2011, https://www.ksl.com/?sid=18282965

How Chinooks Occur, Wikipedia, https://en.wikipedia.org/wiki/Chinook_wind#How_Chinooks_occur