The mean square error (MSE) of a lagged ensemble of monthly forecasts of the Niño 3.4 index from the Climate Forecast System (CFSv2) is examined with respect to ensemble size and configuration. Although the real‐time forecast is initialized 4 times per day, it is possible to infer the MSE for arbitrary initialization frequency and for burst ensembles by fitting error covariances to a parametric model and then extrapolating to arbitrary ensemble size and initialization frequency. Applying this method to real‐time forecasts, we find that the MSE consistently reaches a minimum for a lagged ensemble size between one and eight days, when four initializations per day are included. This ensemble size is consistent with the 8–10 day lagged ensemble configuration used operationally. Interestingly, the skill of both ensemble configurations is close to the estimated skill of the infinite ensemble. The skill of the weighted, lagged, and burst ensembles are found to be comparable. Certain unphysical features of the estimated error growth were tracked down to problems with the climatology and data discontinuities.
2017 | Geophysical Research Letters 44(9), 4304-4312, 2017
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Climate models have consistently projected a drying trend in the southwestern United States, aiding speculation of increasing dust storms in this regi...
2017 | Journal of Advances in Modeling Earth Systems 9(2), 1473-1487, 2017
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Numerical solution of the one-dimensional Richards' equation is the recommended method for coupling groundwater to the atmosphere through the vadose z...
2017 | Journal of Geophysical Research: Space Physics 122(8), 9056-9067, 2017
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Since the mid-1970s, the Defense Meteorological Satellite Program (DMSP) spacecraft have operated instruments for monitoring the space environment fro...
2017 | Journal of Advances in Modeling Earth Systems 9(8), 3045-3068, 2017
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The quasi-geostrophic omega equation has been used extensively to examine the large-scale vertical velocity patterns of atmospheric systems. It is der...
2017 | Journal of Geophysical Research: Space Physics 122(8), 9068-9079, 2017
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We have developed a method for reprocessing the multidecadal, multispacecraft Defense Meteorological Satellite Program Special Sensor Magnetometer (DM...
2016 | Journal of Advances in Modeling Earth Systems 8(4), 1969-1985, 2016
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In this study, a one-dimensional (1-D) thermal diffusion lake model within the Weather Research and Forecasting (WRF) model was investigated for the L...
2017 | Geophysical Research Letters 44(9), 4107-4115, 2017
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This study investigates some of the benefits and drawbacks of assimilating terrestrial water storage (TWS) observations from the Gravity Recovery and ...
2016 | Journal of Advances in Modeling Earth Systems 8(2), 719-734, 2016
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Assimilation of satellite radiances has been proven to have positive impacts on the forecast skill, especially for regions with sparse conventional ob...
2018 | Journal of Advances in Modeling Systems 10(2), 421-447, 2018
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Detailed, regional climate projections, particularly for precipitation, are critical for many applications. Accurate precipitation downscaling in the ...
2017 | Earth and Space Science 4(5), 314-334, 2017
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While global climate models (GCMs) provide useful projections of near‐surface wind vectors into the 21st century, resolution is not sufficient enoug...
Estuarine environments are continuously being shaped by both natural and anthropogenic sources which directly/indirectly influence the organisms that ...
2017 | Journal of Advances in Modeling Earth Systems 9(2), 870-892, 2017
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Previous modeling work showed that aerosol can affect the position of the tropical rain belt, i.e., the intertropical convergence zone (ITCZ). Yet it ...
2018 | Journal of Advances in Modeling Systems 10(4), 989-1010, 2018
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Parametric uncertainty in convection parameterization is one major source of model errors that cause model climate drift. Convection parameter tuning ...
2017 | Journal of Advances in Modeling Earth Systems 9(1), 291-306, 2017
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We propose a general methodology for determining the lagged ensemble that minimizes the mean square forecast error. The MSE of a lagged ensemble is sh...
2016 | Journal of Advances in Modeling Earth Systems 8(4), 1552-1564, 2016
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Influences of the diurnal cycle on the propagation of the Madden-Julian Oscillation (MJO) convection across the Maritime Continent (MC) are examined u...
2018 | Journal of Advances in Modeling Systems 10(4), 961-970, 2018
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Precipitation is an important climate quantity that is critically relevant to society. In spite of intense efforts, significant precipitation biases r...
2019 | Journal of Advances in Modeling Earth Systems 11(6), 1803-1829, 2019
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Strongly coupled data assimilation (SCDA) views the Earth as one unified system. This allows observations to have an instantaneous impact across bound...
2016 | Journal of Advances in Modeling Earth Systems 8(2), 917-935, 2016
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A number of recent studies investigated impacts of Land-Use and Land-Cover Changes (LULCC) on climate with global Earth System Models (ESMs). Yet many...
2016 | Journal of Advances in Modeling Earth Systems 8(4), 1586-1619, 2016
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The collective effects of convection can influence large-scale circulations that, in turn, act to organize convective activity. Such scale interaction...
2017 | Journal of Advances in Modeling Earth Systems 9(2), 932-948, 2017
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This paper describes a new intermediate global atmosphere model in which synoptic and planetary dynamics including the advection of water vapor are ex...