The present invention relates to bacterial preparations comprising ice nucleation proteins. Such bacterial preparations can in particular be used for the production of snow or rain, for hail suppression or for fog dispersal.

The present invention relates to bacterial preparations comprising ice nucleation proteins. Such bacterial preparations can in particular be used for the production of snow or rain, for hail suppression or for fog dispersal.

The present invention is a deployable climate blanket system for regulating temperature of a water surface, including two or more climate blanket secured one to another, each blanket configured with an interior air-filled cavity and a plurality of weights for maintaining the system into a desired position. When use of the blankets is no longer desired, the blankets can be lowered beneath the water surface so as not to interfere with boat traffic or other surface use of the water.

The present invention is a deployable climate blanket system for regulating temperature of a water surface, including two or more climate blanket secured one to another, each blanket configured with an interior air-filled cavity and a plurality of weights for maintaining the system into a desired position. When use of the blankets is no longer desired, the blankets can be lowered beneath the water surface so as not to interfere with boat traffic or other surface use of the water.

Systems, apparatuses, and methods provide for technology that locates one or more masses of a thunderstorm system, as the thunderstorm system starts to organize and before the thunderstorm system spawns a tornado, and controls a transmission of electromagnetic radiation from the space platform to the one or more masses, wherein the transmitted electromagnetic radiation tracks the one or more masses as the thunderstorm system is starting to organize and rotate, and wherein the transmitted electromagnetic radiation prevents the thunderstorm system from rotating and spawning the tornado.

Systems, apparatuses, and methods provide for technology that locates one or more masses of a thunderstorm system, as the thunderstorm system starts to organize and before the thunderstorm system spawns a tornado, and controls a transmission of electromagnetic radiation from the space platform to the one or more masses, wherein the transmitted electromagnetic radiation tracks the one or more masses as the thunderstorm system is starting to organize and rotate, and wherein the transmitted electromagnetic radiation prevents the thunderstorm system from rotating and spawning the tornado.

A dynamic controllable system 10 for moderating energy absorption at the earth's surface includes a series of panel units 110, 610 mounted above the earth's surface over land and water masses. Each panel unit 110, 610 supports rotatable shafts 112, 612, with panels 100, 600 joined to or integrally formed with the shafts 112, 612. Each panel (forcing) 100, 600 has a radiation reflective surface 102, 602 and a radiation emissive surface 104, 604 opposite the radiation reflective surface 102, 602. The panels 100, 602 are selectively rotated into a predetermined one of a plurality of cardinal positions: reflective, emissive and neutral, or into an intermediate position between two of the cardinal positions. The programmable controller 130 receives various data including top of atmosphere satellite data, air temperature and relative humidity at panel units, weather data, time of day, position of panel units, radiation insolation, and combinations thereof. Responsive to real-time data, both local and regional, the programmable controller directs rotational orientation of panels within the panel units, causing a desired reflection of shortwave and longwave radiation away from the earth's surface.

A dynamic controllable system 10 for moderating energy absorption at the earth's surface includes a series of panel units 110, 610 mounted above the earth's surface over land and water masses. Each panel unit 110, 610 supports rotatable shafts 112, 612, with panels 100, 600 joined to or integrally formed with the shafts 112, 612. Each panel (forcing) 100, 600 has a radiation reflective surface 102, 602 and a radiation emissive surface 104, 604 opposite the radiation reflective surface 102, 602. The panels 100, 602 are selectively rotated into a predetermined one of a plurality of cardinal positions: reflective, emissive and neutral, or into an intermediate position between two of the cardinal positions. The programmable controller 130 receives various data including top of atmosphere satellite data, air temperature and relative humidity at panel units, weather data, time of day, position of panel units, radiation insolation, and combinations thereof. Responsive to real-time data, both local and regional, the programmable controller directs rotational orientation of panels within the panel units, causing a desired reflection of shortwave and longwave radiation away from the earth's surface.

Provided is a method for analyzing an effect of a hygroscopic seeding material sprayed through an airborne cloud seeding experiment on ground aerosol concentrations, including the steps of: inputting information of meteorological fields and seeding spraying of the airborne cloud seeding experiment to a numerical cloud seeding model to execute a numerical simulation; calculating a mass concentration of the hygroscopic seeding material on ground, based on results of the numerical simulation; and calculating a contribution degree of the hygroscopic seeding material to mass concentrations of aerosols, based on comparison between the calculated mass concentration of the hygroscopic seeding material and the mass concentrations of the aerosols observed on an execution date of the airborne cloud seeding experiment.

Provided is a method for analyzing an effect of a hygroscopic seeding material sprayed through an airborne cloud seeding experiment on ground aerosol concentrations, including the steps of: inputting information of meteorological fields and seeding spraying of the airborne cloud seeding experiment to a numerical cloud seeding model to execute a numerical simulation; calculating a mass concentration of the hygroscopic seeding material on ground, based on results of the numerical simulation; and calculating a contribution degree of the hygroscopic seeding material to mass concentrations of aerosols, based on comparison between the calculated mass concentration of the hygroscopic seeding material and the mass concentrations of the aerosols observed on an execution date of the airborne cloud seeding experiment.