Improving snowfall forecasting by accounting for the climatological variability of snow density

Accurately forecasting snowfall is a challenge. In particular, one poorly understood component of snowfall forecasting is determining the snow ratio. The snow ratio is the ratio of snowfall to liquid equivalent and is inversely proportional to the snow density. In a previous paper, an artificial neu...

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Veröffentlicht in:Weather and forecasting 2006-02, Vol.21 (1), p.94-103
Hauptverfasser: WARE, Eric C, SCHULTZ, David M, BROOKS, Harold E, ROEBBER, Paul J, BRUENING, Sara L
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container_start_page 94
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creator WARE, Eric C
SCHULTZ, David M
BROOKS, Harold E
ROEBBER, Paul J
BRUENING, Sara L
description Accurately forecasting snowfall is a challenge. In particular, one poorly understood component of snowfall forecasting is determining the snow ratio. The snow ratio is the ratio of snowfall to liquid equivalent and is inversely proportional to the snow density. In a previous paper, an artificial neural network was developed to predict snow ratios probabilistically in three classes: heavy (1:1 < ratio < 9:1), average (9:1 ≤ ratio ≤ 15:1), and light (ratio > 15:1). A Web-based application for the probabilistic prediction of snow ratio in these three classes based on operational forecast model soundings and the neural network is now available. The goal of this paper is to explore the statistical characteristics of the snow ratio to determine how temperature, liquid equivalent, and wind speed can be used to provide additional guidance (quantitative, wherever possible) for forecasting snowfall, especially for extreme values of snow ratio. Snow ratio tends to increase as the low-level (surface to roughly 850 mb) temperature decreases. For example, mean low-level temperatures greater than −2.7°C rarely (less than 5% of the time) produce snow ratios greater than 25:1, whereas mean low-level temperatures less than −10.1°C rarely produce snow ratios less than 10:1. Snow ratio tends to increase strongly as the liquid equivalent decreases, leading to a nomogram for probabilistic forecasting snowfall, given a forecasted value of liquid equivalent. For example, liquid equivalent amounts 2.8–4.1 mm (0.11–0.16 in.) rarely produce snow ratios less than 14:1, and liquid equivalent amounts greater than 11.2 mm (0.44 in.) rarely produce snow ratios greater than 26:1. The surface wind speed plays a minor role by decreasing snow ratio with increasing wind speed. Although previous research has shown simple relationships to determine the snow ratio are difficult to obtain, this note helps to clarify some situations where such relationships are possible.
doi_str_mv 10.1175/waf903.1
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Snow ratio tends to increase as the low-level (surface to roughly 850 mb) temperature decreases. For example, mean low-level temperatures greater than −2.7°C rarely (less than 5% of the time) produce snow ratios greater than 25:1, whereas mean low-level temperatures less than −10.1°C rarely produce snow ratios less than 10:1. Snow ratio tends to increase strongly as the liquid equivalent decreases, leading to a nomogram for probabilistic forecasting snowfall, given a forecasted value of liquid equivalent. For example, liquid equivalent amounts 2.8–4.1 mm (0.11–0.16 in.) rarely produce snow ratios less than 14:1, and liquid equivalent amounts greater than 11.2 mm (0.44 in.) rarely produce snow ratios greater than 26:1. The surface wind speed plays a minor role by decreasing snow ratio with increasing wind speed. Although previous research has shown simple relationships to determine the snow ratio are difficult to obtain, this note helps to clarify some situations where such relationships are possible.</abstract><cop>Boston, MA</cop><pub>American Meteorological Society</pub><doi>10.1175/waf903.1</doi><tpages>10</tpages><oa>free_for_read</oa></addata></record>
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source American Meteorological Society; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection
subjects Artificial neural networks
Atmospheric models
Datasets
Density
Earth, ocean, space
Equivalence
Exact sciences and technology
External geophysics
Extreme values
Extreme weather
Forecasting
Low temperature
Mean
Meteorology
Neural networks
Nomograms
Precipitation
Ratios
Snow
Snow density
Snowfall
Soundings
Statistical analysis
Surface wind
Temperature
Water in the atmosphere (humidity, clouds, evaporation, precipitation)
Weather analysis and prediction
Weather forecasting
Wind
Wind speed
title Improving snowfall forecasting by accounting for the climatological variability of snow density
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