Lake Effect Snow Essay

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INTRODUCTION
The winter season can be a major hassle for some people while others just have to deal with a slight cool down in temperatures. Over the northern portions of the country, people are faced to deal with the harsh conditions that Mother Nature has in store. Some winter seasons are less brutal than others. Besides the typical storm systems that come through the area and drop different types of precipitation whether it is snow, sleet, or freezing rain, there’s another weather event that affects not everyone in the country, but primarily around the Great Lakes. Lake effect snow is a very interesting mesoscale convective phenomenon that occurs mostly during the heart of the winter season and adds greatly to the annual snowfall that areas …show more content…

A study was done to understand the effects of thundersnow within lake effect snow events which took place between 1995 through 2007. What the study observed was that the majority of cloud to ground lightning occurred in lake effect storms during the late fall and early winter months. Twenty-seven percent of storms however occurred between the January through March period. BUFKIT was used in this study to determine the environment that would be required for lightning to occur in these storms. “The presence of the layer from -10 to -25 C within the predicted lake-effect cloud layer (lake-induced LCL to EL analyzed within BUFKIT) appears to be necessary, but not sufficient, condition for CG lightning to occur; values over 500 J/kg of lake induced CAPE much also be present for CG lightning initiation.” (Vol 48, 900). Another requirement of necessary conditions for lighting to occur is that greater heights of the -10 isotherms that are greater than a kilometer above ground level are “also conductive to lake effect lightning because this condition allows more graupel to form in the warmer cloud.” (Vol 48 900). Having a higher equilibrium level greater than 3.6km will allow greater cloud depth to develop convection. Minimal wind shear and more signalized snow bands instead of multiple bands will enhance the …show more content…

While model grid spacing’s were becoming less sporadic going form 15-20 to 38 grid points over the great lakes, the model resolution was still not sufficient enough to pick up on this type of event. Forecasters wanted a high resolution mesoscale model but the model is only as good as the data that is incorporated into it. There needed to be vastly improved data and they “called for a high resolution (temporal and spatial) observational network that included automatic weather stations able to report surface temperature, pressure, and precipitation in real time; wind profilers able to estimate wind speed and direction at various levels; and a new Doppler radar system that could locate snow bands 100 kilometers away.”

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