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Impact of Ural blocking on winter warm Arctic-cold Eurasian anomalies. Part...
In Part I of this study, the Ural blocking (UB)-induced amplification role of winter warm Arctic–cold Eurasian (WACE) anomalies has been examined. It was found that the long-...- publication PDF
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A characterization of the present-day arctic atmosphere in CCSM4
Simulation of key features of the Arctic atmosphere in the Community Climate System Model, version 4 (CCSM4) is evaluated against observational and reanalysis datasets for the...- publication PDF
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The practical predictability of storm tide from tropical cyclones in the...
The potential for storm surge to cause extensive property damage and loss of life has increased urgency to more accurately predict coastal flooding associated with landfalling...- publication PDF
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Electromagnetic ducting in the near-shore marine environment: Results from...
We used the observations from the east coast of the USA and model simulations to elicit marine atmospheric surface layer (MASL) processes that controlled the spatial variability...- publication PDF
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Features of the F3 layer in the low-latitude ionosphere at sunset
The F₃ layer is a common feature within ±10° of the magnetic equatorial ionosphere in the daytime. According to Balan et al. (1998) the F₃ layer occurs mainly during the...- publication PDF
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Simulations of the West African monsoon with a superparameterized climate...
The West African monsoon seasonal cycle is simulated with two coupled general circulation models: the Community Climate System Model (CCSM), which uses traditional convective...- publication PDF
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Impacts of targeted AERI and Doppler lidar wind retrievals on short-term...
The ability of Atmospheric Emitted Radiance Interferometer (AERI) and Doppler lidar (DL) wind profile observations to impact short-term forecasts of convection is explored by...- publication PDF
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Adiabatic evolution of cloud droplet spectral width: A new look at an old problem
Spectral width of the cloud droplet spectrum is important for radiative properties and drizzle/rain development in warm ice-free clouds. We use an adiabatic rising parcel model...- publication PDF
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Responses of the thermosphere and ionosphere system to concurrent solar...
We conducted numerical simulations to examine dayside thermosphere and ionosphere responses to concurrent solar flares and a geomagnetic storm during 6–11 September 2017, as...- publication PDF
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Convective injection into stratospheric intrusions
Stratospheric intrusions (tropopause folds) are known to be major contributors to stratosphere-troposphere exchange. The specific mixing processes that lead to irreversible...- publication PDF
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Isotropization at small scales of rotating helically driven turbulence
We present numerical evidence of how three-dimensionalization occurs at small scale in rotating turbulence with Beltrami (ABC) forcing, creating helical flow. The Zeman scale lΩ...- publication PDF
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A probabilistic climatology-based analogue intensity forecast scheme for...
In this article, we develop an objective probabilistic climatology-based intensity forecast (PCIF) scheme for tropical cyclones (TCs) over the northwestern Pacific region based...- publication PDF
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Numerical impacts on tracer transport: Diagnosing the influence of dynamical...
Accurate representation of stratospheric trace gas transport is important for ozone modeling and climate projection. Intermodel spread can arise from differences in the...- publication PDF
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The role of humidity in determining future electricity demand in the...
Co-occurrence of high relative humidity levels and high temperatures can increase human discomfort, thereby affecting electricity requirements for space cooling. While relative...- publication PDF
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Behavior of the F₂ peak ionosphere over the South Pacific at dusk during...
The six-satellite Constellation Observing System for Meteorology, Ionosphere and Climate (COSMIC) mission makes routine ionospheric measurements over the entire globe using...- publication PDF
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Numerical simulation of mountain waves over the Southern Andes. Part II:...
A companion paper by Lund et al. employed a compressible model to describe the evolution of mountain waves arising due to increasing flow with time over the southern Andes,...- publication PDF
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The Brewer-Dobson circulation in CMIP6
The Brewer-Dobson circulation (BDC) is a key feature of the stratosphere that models need to accurately represent in order to simulate surface climate variability and change...- publication PDF
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Sydney 2000 Forecast Demonstration Project: Convective storm nowcasting
Five of the nowcasting systems that were available during the Sydney 2000 Forecast Demonstration Project (FDP) were selected for evaluation. These systems, from the United...- publication PDF
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Long-term continuous atmospheric CO₂ measurements at Baring Head, New Zealand
We present descriptions of the in situ instrumentation, calibration procedures, intercomparison efforts, and data filtering methods used in a 39-yr record of continuous...- publication PDF
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The 6.5-day wave and its seasonal variability in the middle and upper atmosphere
The zonal wave number 1 planetary wave of period near 6.5 days is a robust feature in the mesosphere and lower thermosphere (MLT) region with prominent seasonal variability as...- publication PDF