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Development and validation of the whole atmosphere Community Climate Model...
Key developments have been made to the NCAR Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension (WACCM-X). Among them, the most important are the...- publication PDF
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Origin of interannual variability in global mean sea level
The two dominant drivers of the global mean sea level (GMSL) variability at interannual timescales are steric changes due to changes in ocean heat content and barystatic changes...- publication PDF
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Turbulent collision-coalescence in maritime shallow convection
This paper discusses cloud simulations aiming at quantitative assessment of the effects of cloud turbulence on rain development in shallow ice-free convective clouds. Cloud...- publication PDF
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Decadal disruption of the QBO by tropical volcanic supereruptions
The Los Chocoyos (14.6 degrees N, 91.2 degrees W) supereruption happened similar to 75,000 years ago in Guatemala and was one of the largest eruptions of the past 100,000 years....- publication PDF
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The role of diurnal solenoidal circulation on propagating rainfall episodes...
In this case study, numerical simulations using the Weather Research and Forecasting model (WRF) are performed for 3-4 May 2002, in which two propagating rain episodes occurred...- publication PDF
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High-latitude cooling associated with landscape changes from North American...
Fires in the boreal forests of North America are generally stand-replacing, killing the majority of trees and initiating succession that may last over a century. Functional...- publication PDF
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Temperature trends in the NARCCAP regional climate models
The skill of six regional climate models (RCMs) in reproducing short-term (24-yr), observed, near-surface temperature trends when driven by reanalysis is examined. The RCMs are...- publication PDF
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Incorporating misclassification error in skill assessment
It is desirable to account for misclassification error of meteorological observations so that the true skill of the forecast can be assessed. Errors in observations can occur,...- publication PDF
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A global scale mechanistic model of photosynthetic capacity (LUNA V1.0)
Although plant photosynthetic capacity as determined by the maximum carboxylation rate (i.e., Vc, max25) and the maximum electron transport rate (i.e., Jmax25) at a reference...- publication PDF
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A framework to understand the asymptotic properties of Kriging and splines
Kriging is a nonparametric regression method used in geostatistics for estimating curves and surfaces for spatial data. It may come as a surprise that the Kriging estimator,...- publication PDF
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Empirical orthogonal function analysis and modeling of the ionospheric peak...
The ionospheric peak electron density height (hm) is one of the most important ionospheric parameters characterizing high-frequency radio wave propagation conditions. In this...- publication PDF
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The thermoinsulation effect of snow cover within a climate model
We use a state of the art climate model (CAM3-CLM3) to investigate the sensitivity of surface climate and land surface processes to treatments of snow thermal conductivity. In...- publication PDF
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Modeling hydroclimatic change in southwest Louisiana rivers
We applied the newly developed WRF-Hydro model to investigate the hydroclimatic trend encompassing the three basins in Southwest Louisiana as well as their connection with...- publication PDF
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To assess marine cloud brightening's technical feasibility, we need to know...
This article does not have an abstract or article summary.- publication PDF
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Compilation of climate data from heterogeneous networks across the Hawaiian Islands
Long-term, accurate observations of atmospheric phenomena are essential for a myriad of applications, including historic and future climate assessments, resource management, and...- publication PDF
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The data conservancy instance
Digital research data can only be managed and preserved over time through a sustained institutional commitment. Research data curation is a multi-faceted issue, requiring...- publication PDF
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Formaldehyde evolution in US wildfire plumes during the Fire Influence on...
Formaldehyde (HCHO) is one of the most abundant non-methane volatile organic compounds (VOCs) emitted by fires. HCHO also undergoes chemical production and loss as a fire plume...- publication PDF
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Evaluation of boundary-layer and urban-canopy parameterizations for...
The simulated winds within the urban canopy of landfalling tropical cyclones are sensitive to the representation of the planetary boundary and urban canopy layers in numerical...- publication PDF
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The role of flare-driven ionospheric electron density changes on the doppler...
Trans-ionospheric high frequency (HF: 3-30 MHz) signals experience strong attenuation following a solar flare-driven sudden ionospheric disturbance (SID). Solar flare-driven HF...- publication PDF
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A global climatology of wind-wave interaction
Generally, ocean waves are thought to act as a drag on the surface wind so that momentum is transferred downward, from the atmosphere into the waves. Recent observations have...- publication PDF
