2021
DOI: 10.1016/j.atmosres.2021.105673
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Seasonal variation of the surface wind forecast performance of the high-resolution WRF-RTFDDA system over China

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Cited by 12 publications
(9 citation statements)
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References 38 publications
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“…The results of our analysis show that dust forecasts produced by a mesoscale model in which simulated emissions are the only source of elevated dust (with no elevated dust in the initial conditions) may show different error growth patterns than those found in meteorological forecast variables (e.g., wind, temperature) following data assimilation. Our wind-speed verification against surface observations, as well as verification of WRF-RTFDDA against surface and upper observations found in literature (e.g., Wyszogrodzki et al, 2013;Pan et al, 2021) illustrates this fact. In Figure 2 and in Pan et al (2021) error growth starts at the very few hours after free forecast initialization following data assimilation, and may saturate or continue to grow with free forecast lead time.…”
Section: Discussionsupporting
confidence: 85%
See 1 more Smart Citation
“…The results of our analysis show that dust forecasts produced by a mesoscale model in which simulated emissions are the only source of elevated dust (with no elevated dust in the initial conditions) may show different error growth patterns than those found in meteorological forecast variables (e.g., wind, temperature) following data assimilation. Our wind-speed verification against surface observations, as well as verification of WRF-RTFDDA against surface and upper observations found in literature (e.g., Wyszogrodzki et al, 2013;Pan et al, 2021) illustrates this fact. In Figure 2 and in Pan et al (2021) error growth starts at the very few hours after free forecast initialization following data assimilation, and may saturate or continue to grow with free forecast lead time.…”
Section: Discussionsupporting
confidence: 85%
“…Our wind-speed verification against surface observations, as well as verification of WRF-RTFDDA against surface and upper observations found in literature (e.g., Wyszogrodzki et al, 2013;Pan et al, 2021) illustrates this fact. In Figure 2 and in Pan et al (2021) error growth starts at the very few hours after free forecast initialization following data assimilation, and may saturate or continue to grow with free forecast lead time. This is expected as errors in the initial conditions propagate into the forecasts and the positive impact of assimilation reduces as the atmospheric state evolves.…”
Section: Discussionsupporting
confidence: 85%
“…Negative biases occur in a few windy mountainous areas of Xinjiang, northern Inner Mongolia, and the Qinghai-Tibet Plateau (Lew, 2000). Previous studies have reported similar SWS prediction errors in other regions (Duan et al, 2018;Feng, Sun, & Zhang, 2020;Misaki et al, 2019;Pan et al, 2021;Shimada et al, 2011;Wyszogrodzki et al, 2013).…”
mentioning
confidence: 70%
“…Wave height (Buoy), wind speed [38] Wave height/period, wind speed/direction, sea level pressure, gust speed, air pressure, Sea surface temperature, buoy data [39] Mean wave period (wave buoy data) [37] Offshore wind speed (light detection and ranging and seashore meteorological mast) [40] Wave height/period/direction (buoy station from NOAA) [41] Daily ocean wave height prediction [42] Wind power generation [43] Wind power forecast [44] Wind speed forecasting [45][46][47][48] Wind forecasting [49] Wind farm cluster power prediction [50] Surface wind forecast [51] Prediction of directly gained or measured parameters are more flexible and easier to achieve than calculated power. However, indirect factors such as temperature, salinity, pressure and precipitation might be used for forecasting and prediction or the exploration of correlations [13].…”
Section: Applicationsmentioning
confidence: 99%