We set the scales of the point value for each of the selected factors. The greatest differentiation on the sides of the horizon has solar radiation, since in the latitudes of Moscow its change is extremely large.
In addition, its role as a hygienic factor is also the most significant. Suppose that this factor, as a presenter, is estimated on a 5-point scale. The factors of the heat background of the wind are difficult to evaluate on a 5-point scale, since for such an assessment there is not enough data, and the importance of these factors in Moscow is less. Therefore, we will accept 3-point scales for them.
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Solar radiation is also evaluated taking into account the overheating factor during the orientation to the SWR, but mainly taking into account the deficiency of insolation during orientation on s, SZ and SZ. The wind regime is evaluated from the calculation that the most unfavorable winds both in January and in July (more than 5 m/s) blow from the north, and in January also from the southeast. The remaining sides of the horizon are equal in quality of wind exposure. Summing up points for each orientation, we get an absolute amount of points that helps determine the “place” of each rumba, evaluate it in points. A rose of assessment of the horizon for a number of factors for Moscow was built by the amount of points. What typological characteristics of the dwelling can be revealed on the basis of such an assessment? The disclosure of the space of residential groups is preferably south, as well as to the southeast, provided that the green stripes are protected from winds, and to the south-west, subject to protection against overheating by ventilating courtyards and the corresponding landscaping. The best orientation of the dwellings is southern and southeast. Eastern, southwest and western to them, northern-even more so. With western and southwestern orientation, it is advisable to protect the windows from the sun in the summer.
Architectural analysis of microclimate – assessment of local conditions – provides for an assessment of the microclimatic variability of the main elements of the climate under the influence of the underlying surface of the city or construction site. Analysis can be carried out in relation to the landscape microclimate or to the development microclimate. The methods proposed below should be used for urban territories with a crossed terrain. A microclimatic assessment of cities located in mountainous areas, or near large reservoirs requires field survey.