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Hardiness zone
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A hardiness zone is shown on the scale to our right; or usually shown on a map (scroll below to see yours). These zones show a geographically-defined area in which a specific category of plant life is capable of growing, as defined by climatic conditions, including it's ability to withstand the minimum temperatures of the zone.
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Encyclopedia
A hardiness zone is shown on the scale to our right; or usually shown on a map (scroll below to see yours). These zones show a geographically-defined area in which a specific category of plant life is capable of growing, as defined by climatic conditions, including it's ability to withstand the minimum temperatures of the zone. The zones were first developed by the United States Department of Agriculture (USDA) and have subsequently been adopted elsewhere.
Benefits and criticisms
The hardiness zones are informative in so far that extremes of winter cold are a major determining factor in whether a plant species can be cultivated outdoors at a particular location. However, the USDA hardiness zones have a number of drawbacks.
Possibly the largest drawback is that they do not incorporate summer heat levels into the zone determination. Sites which may have the same mean winter minima, but markedly different summer temperatures, will still be accorded the same hardiness zone. An extreme example is the Shetland Islands and southern Alabama, which are both on the boundary of zones 8 and 9 and share the same winter minima, but very little else in their climates; in summer, the humid subtropical climate of Alabama is about 20 degrees Celsius hotter than the oceanic climate of Shetland, and there are very few plants that can be grown at both locations. Due to its maritime climate, the UK is in AHS Heat Zone 2 (having 1 to 8 days hotter than 30 degrees Celsius) according to the AHS (American Horticultural Society), whereas Alabama is in Zones 7 to 9 (61 to 150 days hotter than 30 degrees Celsius).
Another problem is that the hardiness zones do not take into account the reliability of the snow cover. Snow acts as an insulator against extreme cold temperatures, protecting the root system of hibernating plants. If the snow cover is reliable (then present during the coldest days), the actual temperature to which the roots are exposed is not as low as the hardiness zone number would indicate. As an example, Quebec City in Canada is located in zone 4 but can rely on an important snow cover every year, making it possible to cultivate plants normally rated for zones 5 or 6, whereas in Montreal, located in zone 5, it is sometimes difficult to cultivate plants adapted to the zone because of the unreliable snow cover.
Other factors that affect plant survival but are not considered in hardiness zones are soil moisture, humidity, the number of days of frost, and the risk of a rare catastrophic cold snap. Some risk evaluation – the probability of getting a particularly severe low temperature – often would be more useful than just the average conditions.
Lastly, many plants will survive in a locality but will not flower if the day length is inappropriate or if they require vernalization (a particular duration of low temperature). With annuals, the time of planting can often be adjusted to allow growth beyond their normal geographical range.
An alternative system for describing plant hardiness is to use indicator plants (the USDA also publishes a list of these to go with their map). Common plants with known limits to their range are used. For example, many people will know whether lemons will grow in their locality. If you that, say, Geraldton Wax will grow more or less where lemons will grow, then you have defined the range of Geraldton Wax with some accuracy.
Sunset Books (Associated with Sunset magazine) publishes a series of gardening books that break up climate zones more finely than the USDA zones. Under this system, the US is broken into 45 distinct zones. These zones incorporate ranges of temperatures in all seasons, precipitation, wind patterns, elevation, and length and structure of the growing season.
Britain and Ireland Hardiness Zones
Owing to the moderating effect of the Gulf Stream on the Irish and British temperate maritime climate, Britain, and Ireland even more so, have milder winters than their northerly position suggests. The map shown is a general indication, and does not show that SW Cornwall and coastal S Devon are also zone 10.
This means that the hardiness zones relevant to Britain and Ireland are quite high, from 7 to 10, as shown below.
- 7. In Scotland the Grampians, Highlands and locally in the Southern Uplands and in England the Pennines.
- 8. Most of England, Wales and Scotland, and parts of central Ireland.
- 9. Most of western and southern England and Wales, western Scotland, also a very narrow coastal fringe on the east coast of Scotland and northeast England (within 5 km of the North Sea), London, and most of Ireland.
- 10. Very low lying coastal areas of the southwest of Ireland including the city of Cork, southwest Cornwall, coastal southern Devon (Plymouth-Torbay) and the Isles of Scilly.
Central Europe Hardiness Zones
Central Europe's climate is a good example of a transition from an oceanic climate to a continental climate, which can be noticed immediately when looking at the hardiness zones, which tend to decrease mainly eastwards instead of northwards. Also, the plateaux and low mountain ranges in this region have a significant impact on how cold it might get during winter. Generally speaking, the hardiness zones are high considering the latitude of the region, although not as high as in the UK or even the Faroe Islands where zone 9 extends to 62°N. In Central Europe, the relevant zones decrease from zone 9 at the Belgian and Dutch coasts, as well as some of the Frisian Islands and the island of Heligoland, to zone 6 on the far eastern border between Poland and Belarus. Some isolated, high elevation areas of the Alps and Carpathians may even go down to zone 3 or 4. An extreme example of a cold sink is Funtensee, Bavaria which is in zone 2.
Northern Europe Hardiness Zones
Scandinavia lies at the same latitude as Alaska or Greenland, but the effect of the warm Gulf Stream is even more pronounced here than it is in the British Isles. Save for a very small spot near Karasjok, Norway which is in zone 2, nowhere in the Arctic part of Scandinavia does it get below zone 3. The Faroe Islands, at 62-63°N are in zone 9, the southern coast of Iceland is in zone 8 at 64°N, as are the outer Lofoten Islands at 68°N. Tromso, a coastal city in Norway at 70°N, is in zone 7, and even Longyearbyen, the northernmost true city in the world at 78°N, is still in zone 5. Al these coastal locations have one thing in common, though, which are cold, damp summers, with temperatures rarely exceeding 20°C, or 15°C in Longyearbyen. For this reason, hardiness zones have little meaning in these places, for the same reason as they have little meaning in the Aleutians, which have a similar climate as Iceland or the Faroes despite being 10° further south.
In Sweden and Finland, however, with their warmer and drier summers, it is more valid to use them. In these countries, generally, at sea level to 500 metres, zone 3 is north of the Arctic Circle, including cities like Karesuando, Pajala and Rovaniemi. Kiruna is the big exception here, which being located on a hill above frost traps, is in zone 5. Zone 4 lies between the Arctic Circle and about 64-65°N, with cities such as Oulu and Jokkmokk, Zone 5 (south to 61-62°N) contains cities such as Tampere, Umea and Ostersund. Zone 6 covers the south of mainland Finland, Sweden north of 60°N, and the high plateau of Smaland further south. Here one will find cities such as Gavle, Orebro, Sundsvall and Helsinki. The Aland Islands, as well as coastal Southern Sweden, and the Stockholm area are in zone 7. Finally, Gotland island, and some coastal spots in Blekinge and Skane (In particular Osterlen) are in zone 8. Osterlen also gets a fair amount of summer warmth, because of its close proximity to the European mainland, and it is sheltered by Denmark from the worst of the Atlantic winter storms, giving it a climate which is very similar to the German Rhineland much further south, and allowing interesting vegetation to be grown at 56°N.
Some European cities
And here some hardiness zone data for a few European cities (based on climatological data):
| City | Zone | City | Zone |
|---|
| Amsterdam, The Netherlands | 8-9 | Antwerp, Belgium | 8 | | Berlin, Germany | 8 | Bratislava, Slovakia | 7 | | Bucharest, Romania | 7 | Catania, Italy | 10 | | Copenhagen, Denmark | 7-8 | Cork, Ireland | 10 | | Dublin, Ireland | 9 | Dusseldorf, Germany | 8 | | Edinburgh, Scotland | 8 | Gdansk, Poland | 7 | | Glasgow, Scotland | 9 | Hamburg, Germany | 8 | | Helsinki, Finland | 6 | Istanbul, Turkey | 9 | | Kaliningrad, Russia | 7 | Kiev, Ukraine | 5 | | Krakow, Poland | 7 | Lisbon, Portugal | 10 | | Ljubljana, Slovenia | 7-8 | London, England | 8-9 | | Madrid, Spain | 8 | Malaga, Spain | 10 | | Marseille, France | 10 | Milan, Italy | 8 | | Minsk, Belarus | 5 | Moscow, Russia | 4 | | Munich, Germany | 7 | Murmansk, Russia | 4 | | Nicosia, Cyprus | 10 | Oslo, Norway | 6 | | Oulu, Finland | 4 | Palma, Spain | 10 | | Paris, France | 8-9 | Perm, Russia | 3 | | | Prague, Czech Republic | 7 | Reykjavik, Iceland | 8 | | Riga, Latvia | 6 | Rome, Italy | 10 | | Rovaniemi, Finland | 4 | Saint Petersburg, Russia | 5 | | Sarajevo, Bosnia and Herzegovina | 7 | Santander, Spain | 10 | | Simrishamn, Sweden | 8 | Sofia, Bulgaria | 7 | | Stockholm, Sweden | 7 | Strasbourg, France | 8 | | Tallinn, Estonia | 6 | Torshavn, Faroe | 9 | | Tromso, Norway | 7 | Trondheim, Norway | 6 | | Umea, Sweden | 5 | Vienna, Austria | 7 | | Vilnius, Lithuania | 5-6 | Warsaw, Poland | 6 | | Workuta, Russia | 2 | Zurich, Switzerland | 7 | |
North American hardiness zones
Using as its basis the average annual minimum temperature for a given location, the idea of the USDA map is that it provides an easy guideline for categorizing locations suitable for winter survival of a rated plant in an "average" winter. Since temperatures in the non-coastal-adjacent areas of the continent rarely present a consistent experience from year to year, and occasionally present a major--and often agriculturally devastating--deviation from the average minimum, it is difficult to use this map for much of the country with any long-term reliability, at least in areas close to the margin of a plant's rated hardiness-zone.
The USDA first issued its standardized hardiness zone map in 1960, and revised it in 1965. A new map was issued in 1990, based on U.S. and Canadian data from 1974 through 1986 (and 1971-1984 for Mexico). While the 1990-issue map utilized approximately double the number of stations, it also divided the temperature zones into five-degree a/b zones for greater accuracy. This revised map showed many areas to be suddenly colder than the 1960 map, due largely to a number of severely colder winters in the central and eastern U.S. in the 1974-1986 data-gathering period as opposed to the mid-20th century data-sampling period used in the 1960 map.
The 1990 map shows 10 different zones, each of which represents an area of winter hardiness for the plants of agriculture and our natural landscape. This was revised to introduce zone 11, representing areas that have average annual minimum temperatures above 40°F (4.4°C) and that are therefore essentially frost-free.
Updates
In 2003, a preliminary draft of a new USDA map was produced by the American Horticultural Society (AHS), compiled by Meteorological Evaluation Services Co., Inc. of Amityville, NY, using temperature data collected from July 1986 to March 2002. This was a period of warmer winters than the 1974-1986 period, especially in the eastern U.S.A., and thus the 2003 map placed many areas approximately a half-zone higher (warmer) than the 1990 map had. Many have noted that the map seemed to have drifted closer to the original 1960 map in its overall zone-delineations. While the 2003 AHS draft map purported to show finer detail, for example reflecting urban heat islands by showing the downtown areas of several cities (e.g., Baltimore, Maryland and Washington, DC) as a full zone warmer than outlying areas, the map also did away with the detailed a/b half-zones introduced in the 1990 map, an omission widely criticized by horticulturists and gardeners due to the coarseness of the resulting map. The USDA rejected the AHS 2003 draft map; the agency has stated it is creating its own internal map in an interactive computer format. As of May 2007 the AHS and the National Arboretum websites still present the 1990 map as current.
In addition, the National Arbor Day Foundation in the United States recently completed an extensive updating of U.S. Hardiness Zones in 2006, utilizing essentially the same data used by the AHS, the then-most-recent 15 years’ data available from more than 5,000 National Climatic Data Center cooperative stations across the United States. Once the Foundation analyzed the new data, hardiness zones were revised, generally reflecting warmer recent temperatures in many parts of the country. The Arbor Day Foundation used the updated versions of the same sources of data as had been utilized by the U.S. Department of Agriculture in the creation of its hardiness zone maps. The 2006 map appears to validate the data used in the 2003 draft completed by the AHS. Like the AHS map, it also did away with the more detailed a/b half-zone delineations.
U.S. Cities
Here are the USDA plant hardiness zones for major U.S. cities (based on the draft 2003 map):
| City | Zone | City | Zone |
|---|
| Albuquerque, New Mexico | 7 | Oklahoma City, Oklahoma | 7 | | Anchorage, Alaska | 4 | Omaha, Nebraska | 5 | | Atlanta, Georgia | 8 | Orlando, Florida | 10 | | Baltimore, Maryland | 7-8 | Philadelphia, Pennsylvania | 7 | | Boston, Massachusetts | 6-7 | Phoenix, Arizona | 9 | | Burlington, Vermont | 4 | Pittsburgh, Pennsylvania | 7 | | Chicago, Illinois | 5-6 | Portland, Maine | 5-6 | | Cincinnati, Ohio | 7 | Portland, Oregon | 9 | | Dallas, Texas | 8 | Raleigh, North Carolina | 8 | | Denver, Colorado | 6-7 | St. Louis, Missouri | 7 | | Detroit, Michigan | 5-6 | Salt Lake City, Utah | 7 | | Fairbanks, Alaska | 1 | San Antonio, Texas | 9 | | Honolulu, Hawaii | 11 | San Diego, California | 10-11 | | Houston, Texas | 9 | San Francisco, California | 10 | | Las Vegas, Nevada | 9 | San Jose, California | 10 | | Los Angeles, California | 10-11 | Seattle, Washington | 8 | | Memphis, Tennessee | 8 | Tampa, Florida | 9-10 | | Miami, Florida | 11 | Tucson, Arizona | 8 | | | Minneapolis, Minnesota | 5 | Tulsa, Oklahoma | 7 | | Nashville, Tennessee | 7 | Washington, D.C. | 7-8 | | New Orleans, Louisiana | 9 | Wichita, Kansas | 6 | | New York, New York | 7 | Wilmington, Delaware | 7-8 | |
Australian Hardiness Zones
The Australian continent, though surrounded by ocean, is drier than Europe or North America. Australia numbers its climate zones differently but these can be made roughly equivalent to North American hardiness zones by adding an offset of 6. For example, Australian Zone 3 is roughly equivalent to North America Zone 9. The higher Australian zone numbers have no US equivalents.
- Zone 1 covers the alpine areas of southeastern Australia.
- Zone 2 the tablelands of south east Queensland, New South Wales and Victoria, and the uplands of central Tasmania.
- Zone 3 includes much of the southern half of the continent, except for near the coast.
- Zone 4, because of the warmer seaboard, covers a broad area from coastal Queensland across to Shark Bay and Geraldton in the west, and includes the Mornington Peninsula, areas adjacent to Spencer Gulf and Adelaide, the southwestern coastal zone, Sydney and the north coast of NSW, along with a number of localities dotted all around the southern coast of the continent.
- Zone 5 covers some of the Queensland coast, Western Australia north of Shark Bay, and across the Top End.
- Zone 6 includes the Queensland coast north of Cairns, Cape York Peninsula and the coast of the Northern Territory.
- Zone 7 is mainly restricted to islands off the north coast.
There are problems with classifications of this type: the spread of weather stations is insufficient to give clear zones and too many places with different climates are lumped together. Only 738 Australian stations have records of more than ten years (one station per 98,491 hectares), though more populated areas have relatively fewer hectares per station. Local factors such as aspect, altitude, proximity to the sea also complicate the matter. For example, Mt. Isa has three climatic stations with more than a ten year record. One is in Zone 4a, one in Zone 4b and the other is in Zone 5a. Likewise, Sydney residents can choose between Zones 3a and 4b. Most other cities have similar problems. Different locations in the same city are suitable for different plants, making it hard to draw a meaningful map. There may even be a case for publishing a list of weather stations and their zone classification to allow best use of local conditions.
See also
Bibliography
External links
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