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The sun warms up the air, but it does so unevenly. Because the sun hits different parts of the Earth at different angles, and because Earth has oceans, mountains, and other features, some places are warmer than others. Because of this, we get pockets of warm air and cold air.
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Since gases behave differently at different temperatures, that means you also get pockets with high pressure and pockets with low pressure. In areas of high pressure, the gases in the air are more crowded. In low pressure zones, the gases are a little more spread out.
You should know that cold smoking takes precision and care. There are some very real health risks involved. The good news is that these risks can be mitigated with a proper setup and expert knowledge.
Because hot smoked meat is cooked at temperatures above the danger zone of 140F, the meat does not have to be cured first. The higher temperatures are hot enough to kill off any pathogens that could make you sick.
Salami or smoked salmon are often the first things that spring to mind when we think of cold smoked food. But there is actually a wide range of foods that can be cold smoked, like cheese, for instance.
Sausage and fish (think smoked salmon) are popular cold smoking options, however they carry a higher risk than other types of meat, as they provide just the right conditions for botulism to grow if not handled properly.
I think this is doing everyone a disservice. Information either skims over the inherent dangers, or is so focused on scaring you about the health risks that any budding cold smoking enthusiast is likely to give up on the idea.
If you cure your meat before smoking it (which you most definitely should) the salt will inhibit the growth of bacteria, but will not kill it off completely. To top it off, the temperature at which the meat is kept while cold smoking can encourage bacteria growth if it is not monitored closely.
Due to the high risk of listeria contamination, those who are immunocompromised (for example, the elderly, the chronically ill, and pregnant women) are advised to steer clear of eating cold smoked fish products, even those which are commercially produced.
Cold smoked fish also carries a risk of parasitic infection. Tapeworms, for instance, can make their way into the waterways via runoff from the feces of mammals that live on the land nearby. Cooking would normally kill such parasites, but cold smoking does not.
If you have a Masterbuilt electric smoker, then a cold smoking kit is a nice easy option. This piece of kit attaches to the wood chip loading port of the smoker. You can hope for continuous smoke for up to 6 hours, at a temperature of 100-120F.
Another option is to smoke your meat while it is raw, for a short period of time, taking special care that it does not reach dangerous temperatures. Then cook the meat immediately after the cold smoking process. The purpose of doing things this way is simply to impart a smoky flavor to the meat before cooking it.
This page presents Egypt's climate context for the current climatology, 1991-2020, derived from observed, historical data. Information should be used to build a strong understanding of current climate conditions in order to appreciate future climate scenarios and projected change. You can visualize data for the current climatology through spatial variation, the seasonal cycle, or as a time series. Analysis is available for both annual and seasonal data. Data presentation defaults to national-scale aggregation, however sub-national data aggregations can be accessed by clicking within a country, on a sub-national unit. Other historical climatologies can be selected from the Time Period dropdown list. Data for specific coordinates can be downloaded for in the Data Download page.
Fine tune position: Through Set Horizontal and Set Vertical Position you can add an offset to your zone setting. Vertical and horizontal text alignment are automatically set according to the zone position as well.
SpecView is easy-to-use Supervisory Control and Data Acquisition (SCADA) software for Watlow controllers, including the F4T with INTUITION process controller, ASPYRE power controller and EZ-ZONE controllers, as well as third-party products. Watlow's single point of support for hardware, software and application needs ensures knowledgeable and prompt responses to questions or concerns. This competitively priced package includes field-proven features, many suggested by loyal users. Built-in support and auto-detect for Watlow controllers make setup quick and simple. SpecView from Watlow is ideal for industrial applications with support for bar code readers and touch-screen operation. To try before purchasing, download the SpecView demo.
EZ-ZONE Configurator software allows Watlow EZ-ZONE products like PID controllers, integrated controllers, solid state controllers and others to be configured in one simple process. Its interface is flexible and easier to read than the basic remote user interface (RUI). It operates without requiring purchase of communications options as it uses the standard bus communications protocol that is included with all EZ-ZONE products. The EZ-ZONE Configurator software is available as a free download under the "Literature & Downloads" tab below.
The EZwarePlus & EZware-5000 operator interface software suites create, edit and manage projects for Silver Series and Silver Series EM operator interface terminals (OIT). The programming software features a large variety of built-in screen objects that makes it easy to use and very powerful. When creating screens, the user can call upon extensive graphics libraries, import custom graphics and add numeric displays, entry fields, analog meters, bar graphs and trend graphs with just a few mouse clicks. Screen objects are highly customizable, and the user can create libraries of their own objects for repeat use. The online simulator, Ethernet and universal serial bus (USB) support make testing and downloading fast. Download the EZwarePlus & EZware-5000 operator interface software suite free of charge.
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Western alpine shrubs and meadows can be found between 9,850 and 16,400 ft. These areas tend to have cold winters and mild summers that allow for plant growth. Rhododendron plants cover the lower shrublands, while the alpine meadows, directly above, host a range of flora in the warmer months. Animals found in this region include the snow leopard, Himalayan tahr, musk deer, and pikas.
Sources of earthquakes in Washington and the relative frequency of occurrence. Deep (Benioff zone) earthquakes do not produce tsunamis. However they may trigger landslides that could generate tsunamis. Image adapted from USGS.
The Cascadia subduction zone off the coast of Washington, British Columbia, Oregon, and northern California is the biggest tsunami hazard for Washington State. This very large fault is capable of generating some of the largest and most damaging earthquakes in the world. These earthquakes also cause very large and damaging tsunamis. The following series of diagrams shows how tsunamis are created along the Cascadia subduction zone.
Other faults in Washington, such as the Seattle Fault, can also move the ocean floor and cause tsunamis. The Seattle Fault is known to have had an earthquake event that directly produced a tsunami (see Atwater and Moore, 1992), and other crustal faults (Tacoma Fault and Darrington-Devils Mountain fault zone, for example) could produce tsunamis (Williams and others, 2000).
Tsunamis generated from earthquakes at other subduction zones and faults around the Pacific Ocean have the potential to impact our shores. Of the numerous historical events that have occurred, only the 1964 Alaska earthquake-generated tsunami has caused damage to the Washington coast. Most tsunami alert messages received for Washington are related to earthquakes in Alaska. You can read more about the impacts of the 1964 Alaska tsunami here.
The public must know how to recognize and respond to natural tsunami warnings, such as ground shaking from an earthquake. Examples of local tsunami threats in Washington are tsunamis generated from earthquake events on the Cascadia subduction zone or local crustal faults such as the Seattle or Tacoma faults.
These signs tell you that you are in a place that is especially at risk for tsunamis. Washington has the second highest seismic risk in the United States (behind California) due to the presence of numerous crustal faults and a subduction zone offshore.
Dead cedar snags along the Copalis River. Here the land subsided several feet during the 1700 Cascadia subduction zone earthquake.Illustrated example of how earthquake subsidence leads to tree death, followed by sediment deposition. Image modified from a diagram by Brian Atwater, USGS.When tsunamis inundate a coastline, they may leave behind distinct sediment deposits. These deposits are typically layers of sand and other debris that are carried up and deposited on land by the force of the tsunami waves. These deposits are found in marshes and near-tidal areas where the sand gets trapped in the root systems of plants. The thicknesses of these deposits reflect the size of the tsunami and the probable tsunami source.Diagram of how tsunami deposits are created.Photo of tsunami deposits (sand layers with silty clays above and below) at Discovery Bay, WA. Four tsunami deposits visible in photo include an inferred AD 1700 sand layer that was later disturbed by marsh restoration projects, a sand layer dated at 630 to 560 radiocarbon years BP (Garrison-Laney and Miller, 2017), and two older sand layers beneath. The topmost mud layer was deposited in 2006, following marsh restoration. Photo by Carrie Garrison-Laney (Washington Sea Grant).The map below shows the locations of tsunami deposits along the Pacific Northwest coastline. Deposits found on the outer coast are dominantly from the Cascadia subduction zone, while those within Puget Sound are typically from local crustal faults such as the Seattle fault.Locations of identified tsunami deposits. Figure adapted from a map by Carrie Garrison-Laney (WA Sea Grant). 2ff7e9595c
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