The purpose of my research to use the dense coverage of seismic stations provided by the Transportable Array (TA) to identify and characterize local weather systems such that they can be differentiated from hurricanes. We utilize seismic and barometric data from the TA across the northeastern United States in 2014, and examine correlations between the microseismic power and the proximity of local weather systems. We also analyze differences in microseism signals related to local weather coming from different directions. This research will be important for analyzing whether a microseism signal is a tropical storm or local weather when reanalyzing historical seismograms to bolster storm catalogs.