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Spectropolarimetric inversions of the He I 10830: A multiplet in an active...
Full Stokes spectropolarimetric data (in the 10830 A region) of an active region filament were obtained in July 2005 using the Tenerife Infrared Polarimeter instrument. The...- publication PDF
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Effects of parameterized diffusion on simulated hurricanes
In this study the authors analyze and interpret the effects of parameterized diffusion on the nearly steady axisymmetric numerical simulations of hurricanes presented in a...- publication PDF
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Spectral analysis of ionospheric electron density and mesospheric neutral...
We use two-dimensional spectral analysis method to extract diurnal eastward zonal wavenumber 3 (E3) and westward zonal wavenumber 2 (W2) nonmigrating tide in the mesospheric...- publication PDF
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Modeling of cloud microphysics: Can we do better?
Representation of cloud microphysics is a key aspect of simulating clouds. From the early days of cloud modeling, numerical models have relied on an Eulerian approach for all...- publication PDF
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Assimilating precipitation data via fullâhydrometeor scheme in WRF...
The full‐hydrometeor four‐dimensional variational (4D‐Var) assimilation scheme in the Weather Research and Forecasting (WRF) model, based on the WRF...- publication PDF
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Evolution of ocean heat content related to ENSO
As the strongest interannual perturbation to the climate system, El Nino-Southern Oscillation (ENSO) dominates the year-to-year variability of the ocean energy budget. Here we...- publication PDF
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NCAR Software Support Library
This manual contains documentation for users of the NCAR Scientific Subroutine Library (NSSL) system file library called ULIB. It is published in three volumes. Each program...- publication PDF
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Probability distributions of land surface wind speeds over North America
Knowledge of the probability distributions of surface wind speeds (SWS) is essential for surface flux estimation, wind power estimation, and wind risk assessments. The two-...- publication PDF
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A note on the top-down and bottom-up gradient functions over a forested site
The dimensionless bottom-up and top-down gradient functions in the convective boundary layer (CBL) are evaluated utilizing long-term well-calibrated carbon dioxide mixing ratio...- publication PDF
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A model intercomparison study of aerosolâcloudâturbulence interactions...
This study presents the first model intercomparison of aerosol‐cloud‐turbulence interactions in a controlled cloudy Rayleigh‐Bénard Convection chamber...- publication PDF
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Magnetic helicity of self-similar axisymmetric force-free fields
In this paper, we continue our theoretical studies addressing the possible consequences of magnetic helicity accumulation in the solar corona. Our previous studies suggest that...- publication PDF
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Data-driven ensemble modeling of equatorial ionospheric electrodynamics: A...
The dayside equatorial ionospheric electrodynamics exhibit strong variability driven simultaneously by highly changeable external forcings that originate from the solar extreme...- publication PDF
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Shallow cumulus representation and its interaction with radiation and...
This article does not have an abstract or article summary.- publication PDF
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Technical description of version 4.5 of the Community Land Model (CLM)
The purpose of this technical note is to describe the biogeophysical and biogeochemical parameterizations and numerical implementation of version 4.5 of the Community Land Model...- publication PDF
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Does ocean coupling matter for the northern extratropical response to...
The question of whether ocean coupling matters for the extratropical Northern Hemisphere atmospheric response to projected late 21st century Arctic sea ice loss is addressed...- publication PDF
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A climatology of hurricane eye formation
This paper presents a climatology of the initial eye formations of a broad set of Atlantic tropical cyclones (TCs) during 1989 - 2008. A new dataset of structure and intensity...- publication PDF
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A comparison of model-based ionospheric and ocean tidal magnetic signals...
Observed tidal geomagnetic field variations are due to a combination of electric currents in the ionosphere, ocean, and their induced counterparts. Using these variations to...- publication PDF
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Boundary value problems for the shallow water equations with topography
Nonviscous shallow water equations with topography are considered in one spatial dimension. The aim is to find boundary conditions which are physically suitable; that is, they...- publication PDF
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Comparison of precipitable water observations in the near tropics by GPS,...
The sensing of precipitable water (PW) using the Global Positioning System (GPS) in the near Tropics is investigated. GPS data acquired from the Central Weather Bureau's Taipei...- publication PDF
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Sensitivity of tropical rainfall to Banda Sea Diffusivity in the Community...
Several observational studies suggest that the vertical diffusivity in the Indonesian marginal seas is an order of magnitude larger than in the open ocean and what is used in...- publication PDF
