Abstract: A method of determining a cloud base through meteorological observation of an atmospheric research aircraft is provided. The method may include collecting meteorological observation information by performing meteorological observation while the atmospheric research aircraft changes a flight altitude, determining a flight altitude that satisfies a plurality of conditions by using the collected meteorological observation information, and determining the determined flight altitude to be a cloud base height. The plurality of conditions may include a first condition in which a liquid water content (LWC) is greater than a first threshold, a second condition in which relative humidity increases or decreases, and a third condition in which a cloud droplet number concentration is greater than a second threshold.

Abstract: The present invention relates to a method for determining a seeding effect area and a non-seeding effect area in accordance with a wind system according to the present invention can use numerical simulation data, radar precipitation data, and ground precipitation data to systematically specify the steps of determining the seeding effect area and the non-seeding effect area in accordance with the wind system. Moreover, the method according to the present invention can easily divide the seeding effect area and the non-seeding effect area according to the physical properties of clouds and quantitatively verify the effectiveness of artificial precipitation experiments conducted by purpose in the future.

Abstract: A method is provided of calculating the total amount of artificial precipitation in a seeded area compared to a non-seeded area, which is capable of increasing the reliability of quantitative determination of seeding effect, observation data, and numerical model prediction data obtained from artificial precipitation experiments, of increasing the amount of water resources through weather modification experiments, of accomplishing various effects (drought reduction, forest fire prevention, fine dust reduction, fog reduction, hail suppression, etc.

Abstract: Provided are a method and system of verifying an increase in precipitation. The precipitation increase verification method includes: obtaining a first piece of observation information from an upwind area after a seeding experiment; obtaining a second piece of observation information from a downwind area; comparing the first piece of observation information with the second piece of observation information, and thus determining whether or not the first piece of observation information and the second piece of observation information fall within a linear scope; and determining that an effect resulting from the seeding experiment can be proved when the first piece of observation information and the second piece of observation information fall within the linear scope.

Abstract: The present invention relates to a method for determining a seeding effect area and a non-seeding effect area in accordance with a wind system according to the present invention can use numerical simulation data, radar precipitation data, and ground precipitation data to systematically specify the steps of determining the seeding effect area and the non-seeding effect area in accordance with the wind system. Moreover, the method according to the present invention can easily divide the seeding effect area and the non-seeding effect area according to the physical properties of clouds and quantitatively verify the effectiveness of artificial precipitation experiments conducted by purpose in the future.

Abstract: A method is provided of calculating the total amount of artificial precipitation in a seeded area compared to a non-seeded area, which is capable of increasing the reliability of quantitative determination of seeding effect, observation data, and numerical model prediction data obtained from artificial precipitation experiments, of increasing the amount of water resources through weather modification experiments, of accomplishing various effects (drought reduction, forest fire prevention, fine dust reduction, fog reduction, hail suppression, etc.

Abstract: Disclosed are a method and apparatus for expressing a seeding line for artificial enhancement of rain in airborne experiments considering cloud water. The method includes calculating average cloud liquid water path (LWP) for each time zone in a target region based on numerical weather prediction (NWP) model data for the target region, calculating an average wind direction and wind velocity in the target region, calculating a middle point and left and right end points of a seeding line candidate which is based on the average wind direction and wind velocity, calculating a seeding line by correcting the seeding line candidate based on a point at which cloud liquid water contents (LWC) is a maximum within upper, lower, left and right selection regions around the middle point and a height at the point, and expressing the seeding line and the height of the seeding line as an optimal seeding line and seeding height if the maximum value of the LWC is greater than 0.