Month: March 2024

In the last week, I’ve driven all the way from western Virginia, where the redbuds are blooming, to Tallahassee, FL, where red clover is everywhere. As I drove through the mountains north of Charlotte NC, I noticed some signs indicating that strong gap winds may blow down the valleys when atmospheric pressure patterns align to produce strong pressure gradients that drive the wind. I have discussed wind before in previous posts (“Who has seen the wind?” and “Does wind chill affect plants?”) so you can find the basics of what causes wind and some of the different kinds of local winds by going to those posts. In today’s article I want to share some different local names for winds and other local weather and invite you to share your own local weather names. Note that this is not a complete list, but I will provide links at the end that prove a bigger sample of all the names that are used around the world to denote different kinds of weather, especially wind.

Local weather names based on topography

Local mountains and valleys can cause a big variety in the types of winds we observe. Generally, these winds can be classified as katabatic winds blowing downhill and anabatic winds blowing uphill. The direction depends on the time of day due to heating but also to large-scale weather patterns that direct the flow of air. Local winds can also occur due to changes in the heights of the ridges so that where the ridges are low, air can spill over the mountains in the gaps between peaks. Winds blowing downslope can also accelerate as they move to lower elevations, increasing their strength. Those winds can be very strong because of the funneling effect of the terrain leading to warnings like the ones I saw on Interstate 77 in the northern North Carolina Mountains. Some of these local winds in other parts of the world are called the Viento Zonda (or Zonda wind) in Argentina, the Williwaw in the Alaskan Panhandle, Karaburan in Central Asia, Chinook wind along the Front Range of the Rocky Mountains in the USA, Mistral in France, and the Warm Braw in the Schouten Islands north of New Guinea. You can read more about each of these by looking online at Wikipedia or other sites (link below). Winds which are affected by topography can provide good sources of steady wind for wind farms.

One of the most interesting large-scale topography-driven winds is the Tehuantepecer in southern Mexico which begins in the Gulf of Mexico (after coming south across North America) as a north wind that crosses the Mexican isthmus and blows through the gap between the Mexican and Guatamalan Mountains. It is so strong that it can be felt as much as 100 miles out to sea. This happens several times a year, especially in winter when the wind is more often from the north, and is amazing to see on https://earth.nullschool.net/ when it happens. In fact, as I am writing this on Thursday (March 28, 2024) it is happening today! How cool is that?

Local weather names based on changes of air mass

Some winds are named for abrupt shifts in atmospheric temperature and humidity when air from a different source region moves in. They can be small-scale changes due to outflows from individual thunderstorms like gust fronts or can be larger-scale changes due to wind blowing an air mass with colder, hotter, or drier characteristics into the area.

Some of the winds associated with drier and dustier conditions occur near desert locations as the wind shifts to bring in air from the desert regions to replace the air that was already there. One of the most common terms for one of these is haboob, which originated in Sudan but is now used in the western U. S. (Haboob basically means “dust storm” in Arabic but sounds a lot more exotic). A haboob is associated with a wall of hot, dusty air that moves into the region from the desert, bringing low visibilities to the region (often resulting in car accidents as drivers caught unawares can be blinded by the sudden change in conditions). Other dry winds include the Khamsin in Egypt and the Red Sea region, the Scirocco in North Africa and the Mediterranean, and the Harmattan in West Africa.

Cold winds include the Blue Norther, a fast-moving cold front that moves in from the north that can send temperature plummeting by 20-30 degrees in a few minutes, the Bora in the Adriatic region, the Khazri in the north Caspian Sea, the Montreal Express in New England, and the Norte in Mexico. In the Southeast US, we have what we call the Wedge, which is a shallow layer of cold air that moves south along the eastern slope of the Appalachian Mountains under northeast flow, bringing clouds, cold weather, and the chance of ice storms to the region in spring. The Wedge is partly due to topography as well, since the cold air is so shallow that it can’t move west over the Appalachian Mountains and thus is forced down to us in parts of the Carolinas and Georgia. Hot dry winds include the Brickfielder in southern Australia, the Leveche in southern Spain, and the Diablo and Santa Ana winds in California, which are also affected by air moving down from the mountains into coastal areas of the state when high pressure dominates the Southwest.

Local winds are associated with thunderstorms

In addition to the wind names associated with topography and change of air quality there are also some names that are tied to smaller weather events like hurricanes and thunderstorms. Those include the Kalbaishakhi in India and Bangladesh, the Bayamo on Cuba’s southern coast, the Pampero in Argentina and Uruguay, the Cordonazo on the west coast of Mexico, and the Borasco in the Mediterranean. Strong winds associated with thunderstorms can cause tremendous damage to gardens, trees, and buildings and can cause problems with flights and road transportation. Since it is spring and we are entering severe weather season for a lot of the US, it’s a good reminder that it does not need to be a tornado to cause significant damage—straight-line winds can be just as severe.

Knowing your local climate is important for gardeners

Anyone who lives for a long time at a location will start to recognize the local weather and climate patterns that govern your local garden conditions. If you are really dedicated, you can even measure these variations. If you know that in certain seasons, you are more likely to experience very dry dusty air, you might consider plants that can survive those conditions with less care. If you live in an area that is subject to frequent strong local winds, you will need to plan your garden to place more wind-resistant plants where the air flow is the strongest or else construct a wind shelter to keep more sensitive plants safe. Buildings can also affect the wind flow and can cause “wind tunnels” where the air is constricted and blows faster in the narrow passage.

Note: For those of you who wonder about the title of this post, Maria (sometimes listed as Mariah) is a fictional wind popularized in “Paint Your Wagon” (Lerner and Lowe, 1951) and by the Kingston Trio (1959). The name may have originated with the 1941 book “Storm” by George R. Stewart according to my colleague Jan Null of Golden Gate Weather Services.

Sources of more local wind information

Here are some websites that have listings of additional local winds, although none of them is a complete list, I am sure.

Wikimedia (with links to most of the individual winds): https://en.wikipedia.org/wiki/List_of_local_winds.

GG Weather: https://ggweather.com/winds.html

U. K. Met Office: https://www.metoffice.gov.uk/weather/learn-about/weather/types-of-weather/wind/wind-names

If you have a local name for the wind or weather in your region, please share it in the comments!

Wherever whitetail deer occur they present a challenge for gardeners. The internet offers abundant advice on this, but too often it is simplistic gardening myth such as scattering human hair or planting garlic.

Historically in deer control literature there have been occasional observations that deer hesitate to enter an area which looks too small or constrained for rapid escape. Finally, it came time to acknowledge and test this theory.

Green Island Preserve and the University of Minnesota Extension set about investigating this possibility through their Regional Sustainable Development Partnership (RSDP) program which provides support to community-benefit projects in partnership with private citizens and organizations. The test site was a 60 acre rewilded forest inside a small northern city. Deer pressure was heavy with resident herd numbers varying from 16-30 animals during the trial.

The first issue was defining a “small space” for testing the theory. In all the literature only one other trial of this concept could be found. It was conducted in Wisconsin with traditionally fenced spaces ranging from 15 ft by 15 ft to 21 ft by 21 ft feet during part of one summer. The Minnesota Green Island Preserve and RSDP trial chose 16 feet by 16 feet based upon the dimensions of manufactured, ridged cattle panels. These panels are 50 inches in height and 16 ft long and tend to be readily available at Fleet or Home stores even in suburban areas. If successful, their advantage would be very easy set-up and portability at a reasonable cost.

What was the result? Over 2 years of trial, this test demonstrated 95% success. Six micro-exclosures were established and planted within forested and forest edge locations in a zone of heavy deer pressure. During an observation period of 730 days, only one instance of deer browse occurred inside a micro-exclosure.

This success rate is more impressive because these fences are not a physical barrier to deer entry. They are strictly a psychological deterrent. This places them in much the same class as flashing lights, sound cannon, water spray, etc., but according to this study’s data, they’re actually more effective. All psychological deterrents have a failure rate dependent on application, monitoring, seasonality, rainfall, and more. But micro-exclosures show a low failure rate, without maintenance. If a deer breach does occur, the solution is simply to make the exclosure appear even smaller. This can be done by stretching rope across the center holding noticeable flagging. It can be lifted off when tending plants.

This is a highly promising discovery which merits further controlled testing by universities and professionals. The Minnesota Green Island Preserve and RSDP trial was specifically targeted to white tail deer predation while other ungulates present browse problems in other geographies. Rabbits were not addressed. However, until further and definitive research is conducted, citizen-scientist gardeners can contribute by testing versions of this method for themselves and adding their data to the general deer-control knowledge base. In using and testing micro-exclosures, gardeners will fare infinitely better than by spreading human hair, interplanting garlic, or buying “ultrasonic” gizmos.

This post was provided by Kent Scheer. Kent is a career sculptor with a side mission for reforestation and environmental compassion. He is the editor of three handbooks on sustainable agriculture resources and owner/ manager of a rewilded pine forest in northern Minnesota created for environmental education and awareness. You can contact Kent at kentscheer@outlook.com.

In the quarter century that I’ve been researching, publishing, and educating on the topic of landscape mulches, one thing has become clear: cardboard should never be used as a mulch. This viewpoint has been of great interest to gardeners; in fact, my earlier post has been the most frequently viewed post since it was published in 2015. I occasionally appended new information to the original post as needed, but the topic deserves an update.

Rather than rehashing what’s been written earlier (which can be found here, here, here, here, and here in addition to the link above), I’m providing information in a Q&A format that might be helpful:

Q: Is there research on using cardboard mulch in home landscapes?

A: Not much. To date, the only peer-reviewed research relevant to landscape soil conditions is our own work published in 2019. The abstract explains the importance of the results to landscape soil health as stated in the abstract (below):

“The orders of magnitude differences in diffusion coefficients among the mulch materials, however, could negatively impact a diverse soil environment such as those found in biologically rich landscapes with higher oxygen demands. Among the mulches tested, wood chips are a preferred method of mulching in terms of providing best gas permeability, particularly in landscape conditions.”

Q: Cardboard has been used as a mulch in agricultural production. Why doesn’t that research support using it in landscapes?

A: The goal in agricultural production is to maximize yield of an annual crop. In contrast, the goal in caring for a permanent landscape is to maintain a healthy soil ecosystem that will support plant life long term. The table below explains these differences in more detail.

Q: Okay, I understand that science doesn’t support using cardboard as a landscape mulch, but what about my vegetable garden? Isn’t the research on agricultural crops relevant there?

A: The research on agricultural production mulches is more relevant if maximizing yield is your most important goal. But your goals may include maintaining a healthy soil ecosystem, reducing the use of pesticides and fertilizers, and other criteria. Are you concerned about the established negative impacts that cardboard and other sheet mulches have on soil life? If so, then sheet mulches are not a good choice compared to chunky, three-dimensional mulches.

Q: I like reusing cardboard packaging as part of organic weed control. Isn’t that a good enough reason to use cardboard?

A: In addition to interfering with water and gas movement into the soil environment, corrugated cardboard has chemical contaminants that you really don’t want in your soil or even your compost pile. Corrugated cardboard contains environmental contaminants including dioxin and PFAs or “forever chemicals.” No gardener should want to introduce more of these widespread contaminants into their landscape or garden soils.

As I’ve been recommending for nearly a quarter century now, the very best mulch to use for treed landscapes is arborist wood chips. There is robust, peer-reviewed science establishing the benefits of arborist chip mulches in controlling weeds, enhancing growth and establishment of landscape plants, and maintaining a functional soil ecosystem. In contrast, sheet mulches such as plastic, weed fabric, and cardboard have demonstrated negative impacts on the long-term health of landscape soils. Any resource that says otherwise is not paying attention to the research-based facts.