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Green Building Bible, Fourth Edition
Green Building Bible, fourth edition (both books)
These two books are the perfect starting place to help you get to grips with one of the most vitally important aspects of our society - our homes and living environment.

PLEASE NOTE: A download link for Volume 1 will be sent to you by email and Volume 2 will be sent to you by post as a book.

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      CommentAuthorfostertom
    • CommentTimeAug 18th 2010 edited
     
    Question for the boffins - help me get clear.

    Wanting to maximise solar radiation intake thro the heating season, so the direct sun that actually comes over the distant valley horizon http://i30.photobucket.com/albums/c301/fostertom/Picture035-033med.jpg is critical - duration, elevation and bearing. Whereas in summer the treetops in leaf would define the horizon, in winter the trees are bare and significant direct radiation will penetrate the branches, down to a lower 'hard' horizon. That will significantly increase the duration of direct sun by about an hour earlier, when the sun is low as it rises.

    In Tas Thermal Modeller, horizons/obstructions can be given varying transparency - semi-penetrable thro most of the winter, becoming opaque as spring arives.

    The question is, what's the principle of estimating the %age of unobstructed radiation, that the bare branches will allow through?
    Is it as simple as estimating what %age of the relevant area remains clear line-of-sight, the remainder blocked by branches and twigs? That can be done from photos.
    Or are there refraction/moire effects at work, the fine screen of obstructions causing incoherence in the radiation?
    Or what?
  1.  
    Fostertom, here is a page with links to PV software, some that will calculate the shadows from a pananoramic photo of your site, might be helpful to you.


    http://www.pvresources.com/en/software.php

    Panorama master - with "Panorama master" you can make exact matched set of photos - base for panorama picture (see also "Horizon" below).

    Horizon - software simulates sun path diagrams for arbitrary latitude.



    Shadows - Shadows is a program used to design sundials and astrolabes and it is very useful also in solar energy engineering. Key points of Shadows:

    Free of charge in its entry level
    Calculates and prints the drawings at real scale
    Simulates, displays and animates the shadow of the style
    Exports drawings as BMP, JPG, EMF and DXF (AutoCAD)
    Offers complete ephemeris of the Sun and draws the Solar Diagram
    Supports plane sundials with polar style of any orientation and reclination, analemmatic sundials, cylindrical and bifilar sundials.

    Languages: fr gb de it es pl


    GOSOL - Das solar + energetische Simulationsprogramm für städtebauliche Planungen.

    Comprehensive tool intended for detailed site analysis, included building shape and vegetation shading analysis. Suitable for urban planning and detailed architecture studies (german language only).
    • CommentAuthorjon
    • CommentTimeAug 19th 2010
     
    A local gravitational field can cause interference to a light particle's waveform and bending of the pathway but is only noticeable with exceptionally fine slits: The sort of obstruction you're talking about is unlikely to have any discernible effect.
    •  
      CommentAuthorSteamyTea
    • CommentTimeAug 19th 2010
     
    Tom

    Are you talking Solar Thermal here, I think you are.
    Leaves, trees or other obstructions can be calculated a number of ways. The reduction in solar input, a reduction in the time at a given input or a combination of both. As most software/models use historic data for the inputs it is almost certain that a mean average is used for the input. Or another way a simple percentage reduction.

    To predict what is really happening is virtually impossible because of the stochastic nature of the weather, but finding out the monthly means is pretty accurate.

    To give an example the 5 charts below are all based on identical data. Just different methodologies.
      Actual Solar and Temp.jpg
    •  
      CommentAuthorSteamyTea
    • CommentTimeAug 19th 2010
     
    More
      Anomolies.jpg
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      CommentAuthorSteamyTea
    • CommentTimeAug 19th 2010
     
    More
      Mean Solar and Temp.jpg
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      CommentAuthorSteamyTea
    • CommentTimeAug 19th 2010
     
    More
      Temp Frequency.jpg
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      CommentAuthorSteamyTea
    • CommentTimeAug 19th 2010 edited
     
    Last
      Solar Frequency.jpg
    •  
      CommentAuthorfostertom
    • CommentTimeAug 19th 2010
     
    Posted By: jonThe sort of obstruction you're talking about is unlikely to have any discernible effect
    meaning that simple %age of bare-branch sky area obstructed by branches and twigs would indeed be right? No subsidiary effects from what looks, from a distance, like a hazy mesh ?
    •  
      CommentAuthorfostertom
    • CommentTimeAug 19th 2010
     
    Posted By: SteamyTeaLeaves, trees or other obstructions can be calculated a number of ways. The reduction in solar input, a reduction in the time at a given input or a combination of both
    That's right, and with a wide-area 3D model, comprising both the 'target' building, the distant horizon (350m distant x 85m high above GrdFl of the building) and closer obstructions (e.g. trees at 50m distance), Tas can run the sunpaths day after day as the season progresses, to see just what duration, elevation and bearing of direct sun radiation the building 'sees', when the sunpath rises above the obstructions.

    Within that, the upper band of the distant (forest) horizon and the whole of the nearby trees are partly transparent while leafless, during most of the time of greatest interest, the heating season. When you say
    Posted By: SteamyTeaAs most software/models use historic data for the inputs it is almost certain that a mean average is used for the input. Or another way a simple percentage reduction
    you're not referring to historic leaf-fall/leaf growth data/dates? I don't think Tas does that, tho why not?

    Your following graphs are interesting, but I'm missing how they apply to %age transparency of bare-branch trees?
  2.  
    Tom,
    Refraction etc only really have much effect when the gaps are similar in size to the wavelength- not likely
    to be at all significant . The 'hazy mesh' effect is probably due to lack of discrimination of small branchlets when viewed at a distance and small wind movements - a good photo should take most of that into account - treat it
    as a mixture of opaque and semi-transparent regions to estimate total throughput.

    Other things of course will have an effect as well - and will be virtually impossible to take account of - e.g.
    reflections from branches - varies due to wetness etc - should increase throughput
    changes in 'branch cover' due to growth and dieback
    snow - will block more light
    Birds!
    All are probably fairly marginal (unless you're dealing with smallish trees that are expected to grow) but also probably more important than esoteric optial effects.
    •  
      CommentAuthorfostertom
    • CommentTimeAug 19th 2010
     
    Thanks Chris.

    The answers look encouraging - same over on AECB -
    Posted By: fostertomsimple %age of bare-branch sky area obstructed by branches and twigs
    it is then, or even a bit better if they're shiny silver birches!

    Amy other comments?
    • CommentAuthorjon
    • CommentTimeAug 19th 2010
     
    <i>meaning that simple %age of bare-branch sky area obstructed by branches and twigs would indeed be right? No subsidiary effects from what looks, from a distance, like a hazy mesh ? </i>

    That's right. The effect of warm air within the tree as the sun shines on it is more likely to have an effect than interference from the branches. Even then, a bit of deflected light is just that and unlikely to make any difference to the averages. Compared to the variability of the cloud cover it's almost an irrelevant consideration. Rest as Chris says.
    •  
      CommentAuthorfostertom
    • CommentTimeAug 19th 2010 edited
     
    Posted By: jonCompared to the variability of the cloud cover it's almost an irrelevant consideration
    But no - it's a major bonus, if what I took to be the skyline (distant forest treetops-in-leaf) is in fact about 3.5o lower in elevation (the hard ground brow, seen thro bare-branch trees).

    Then the sunpath 'sees' the target building considerably earlier in the day, as it rises, albeit partly obstructed by branches and twigs, and albeit weaker in intensity because at lower elevation (longer airpath thro the atmosphere). Especially in the depth of winter, when direct-sun duration is effectively tripled.
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