FAQ: Difference between revisions

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You’ve edited your templates with something like Dreamweaver, and it’s changed the angle brackets on the [[Webtags]] to "&lt ;" and "&gt ;" - you need to change them back to < and >. ''These may look the same when viewed in your browser, but you can see the difference if you 'view source'''  
You’ve edited your templates with something like Dreamweaver, and it’s changed the angle brackets on the [[Webtags]] to "&lt ;" and "&gt ;" - you need to change them back to < and >. ''These may look the same when viewed in your browser, but you can see the difference if you 'view source'''  


Alternatively, if the web templates are listed in [[cumulus.ini]] (and for the first 10 appear on the '''files''' tab of ''Internet'' dialogue of '''Configuation''' menu), the '''Process''' option must be ticked for the web pages generated by Cumulus to have values replacing the [[Webtags]].  Otherwise at each web update, Cumulus will generate web pages the same as the templates.
Alternatively, if the web templates are listed in [[cumulus.ini]] (and for the first 10 appear on the '''files''' tab of ''Internet'' dialogue of '''Configuration''' menu), the '''Process''' option must be ticked for the web pages generated by Cumulus to have values replacing the [[Webtags]].  Otherwise at each web update, Cumulus will generate web pages the same as the templates.




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The international standard states ambient air temperature/humidity is measured at 1.25 metres above ground level, above soil or grass not paving, protected from direct sun radiation (and direct rain), unless you are measuring soil or ground temperatures. The height is important for derived values as an air frost is defined as a temperature below the freezing point for water at this height, and the count of these is a standard reporting requirement in some countries.
The international standard states ambient air temperature/humidity is measured at 1.25 metres above ground level, above soil or grass not paving, protected from direct sun radiation (and direct rain), unless you are measuring soil or ground temperatures. The height is important for derived values as an air frost is defined as a temperature below the freezing point for water at this height, and the count of these is a standard reporting requirement in some countries.


If you are using a ''Fine Offset sensor'', the thin depth of the thermonmeter/hygrometer (transmitter) should face where your console (receiver) is, for maximum transmission strength/distance, with the wide face at right angles to the transmission route. (Although if you use a model requiring a radio time signal, you will probably be trying to optimise that instead).  
If you are using a ''Fine Offset sensor'', the thin depth of the thermometer/hygrometer (transmitter) should face where your console (receiver) is, for maximum transmission strength/distance, with the wide face at right angles to the transmission route. (Although if you use a model requiring a radio time signal, you will probably be trying to optimise that instead).  


== Pressure ==
== Pressure ==