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Aaron R. Naeger, Brian A. Colle, Na Zhou, and Andrew Molthan

partly attributed to initial conditions, in addition to choice of BMP and model resolution. Martin et al. (2018) attributed precipitation deficiencies for AR simulations from the WRF Model to low biases in the low-level water vapor flux. Thus, there remains a strong need to improve forecasts of extreme precipitation events such as ARs in an effort to mitigate flood risk and damage from these storms. The suite of intensive instrumentation deployed during the recent Olympic Mountains Experiment

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