Change in structure of land surface can affect atmospheric boundary layer and formation of internal boundary layer. This will change shear stresses and turbulent boundary layer. Change in low level wind shear and turbulent can affect air craft performance and has potentially adverse effects on flight safety during landing and taking-off stages. In this study, change in land area around Baghdad Airport and its effects on structure of boundary layer and radix layer through summer season (July from years 1985 and 2014) is examined. The examination is done through atmospheric data of radiosonde (at altitude more than 1500 m) and remote sensing by Landsat 5 and 8 images (circular region around airport has radius 3.250 km and the airport is considered the center of this circle). From analysis of hourly wind speed and temperature profile with height observed by radiosonde, change in convective radix layer can be determined at this period resulted from change structure of boundary layer depending on characteristic of landcover used in supervised classification. Building area increases from 18% in 1985 to 41% in 2014. These results enforced by positive values of built up index BI, that showed a decreases in 2014. All these elements changed convective radix layer from less than 500 m in summer 1985 to more than 700 m. There is a large fluctuation in radix layer height depended on convective and friction velocity at 2014 data. Thus indirect change in structure of convective layer will  affect  navigation movement of Baghdad International Airport.

In late 2019 and in Wuhan, a new disease appears, consider as an extension of SARS-COV2 epidemic. This epidemic virus has configured a danger to global health. We studied the effect of some atmospheric elements in Iraq with a number of (COVID-19) infections. In this study daily infections in three regions of Iraq compares with (Tmax-Tmin) and (RH) observed in stations Mosul (represent north region), Baghdad and Rutba (represent middle regions), and Basra (represent south region). It's found that increasing the difference between Tmax and Tmin means more infections, except for the northern province. As for the relative humidity, it is inversely proportional to infections with the correlation coefficient R = -0.6 in Baghdad station, and in the southern province with R = -0.32, and the opposite occurs in the northern province. The results also indicate that increasing the relative humidity to more than 70% was effective in increasing the infections. Solar radiation was studied over the city of Baghdad and its effect on infections because solar radiation contains a large proportion of ultraviolet rays that killed many viruses, the study indicates an inverse relationship because most of the patients are infected in the shade and there is no clear relationship. In late 2019 and in Wuhan, a new decease appears, consider as extension of SARS-COV2 epidemic. This epidemic virus has configured a danger on the global health. We studied the effect of some atmospheric elements in Iraq with number of (COVID-19) infections. At this study daily infections in three regions of Iraq compare with (Tmax-Tmin) and (RH) observed in stations Mosul (represent north region), Baghdad and Rutba (represent middle regions) and Basra (represent south region). It's found that increasing the difference between Tmax and Tmin means more infections, except for the northern province. As for the relative humidity it is inversely proportional to infections with the correlation coefficient R = -0.6 in Baghdad station, and in the southern province with R = -0.32, and the opposite occurs in the northern province. The results also indicate that increasing the relative humidity to more than 70% was effective in increasing the infections. Solar radiation was studied over the city of Baghdad and its effect on infections because solar radiation contains a large proportion of ultraviolet rays that killed many viruses, the study indicates an inverse relationship because most of the patients are infected in the shade and there is no clear relationship.

The paper describes the technical means, methods, and results of experimental studies of the spread of ice-forming agents in the boundary layer of the atmosphere under the action of ground-based aerosol generator NAG-07M. Comparison of the data on sampling by an AVA 3-240-01S probe mounted aboard Vilga-35A aircraft with aerosol propagation calculations using a 3-D SeedDisp model shows 1. The concentration of silver iodide measured in the atmosphere was above background one to a height of 1200 m at distances of 3 to 9 km from the place of the generator installation. 2. The developed SeedDisp numerical model in general qualitatively correctly describes the distribution of silver iodide aerosols in the boundary layer and the free atmosphere under the action of ground-based aerosol generator NAG-07M. Thus, the coefficient of correlation of the measured and calculated by model values of the silver iodide particles concentration in the sub-cloud layer exceeded the value of 0.7.

Cloud cover effects on most other meteorological variables. It effects on the amount of radiation entering the boundary layer of the atmosphere and thus it controls the amount of energy within this range. Evaporation is also an important factor in the formation of clouds and directly affects the energy equation. This study was based on daily data of cloud cover and evaporation values taken from Iraqi meteorological organization and seismology for the period 2000 to 2005 for the city of Baghdad, as well as the solar radiation data of the three components (direct - diffuse - reflected) and the same location and period time period taken from European center of solar energy services for professionals study (soda), monthly and annual rates were calculated to show the correlation between these variables.  To carry out statistical operations and convert the values of the cloud cover to the proportions of eight parts to indicate the proportion of clouds in the sky and drawing diagrams, the results showed that there is a significant effect of the evaporation processes on the formation of the cloud cover. High evaporation values are associated with high values of the cloud cover and have a high positive correlation coefficient value hits (0.74). The results showed that the cloud cover values are inversely proportional to the direct and diffused radiation compounds and have a negative correlation coefficient of  (-0.93). This effect is less on the reflected radiation component. In general, the cloud cover can be used to estimate the values of some other meteorological variables, especially in winter seasons.

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