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Historical Antarctic mean sea ice area, sea ice trends, and winds in CMIP5...
In contrast to Arctic sea ice, average Antarctic sea ice area is not retreating but has slowly increased since satellite measurements began in 1979. While most climate models...- publication PDF
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Energy modulations of magnetospheric ions induced by foreshock...
Although foreshock transients can generate strong magnetospheric Pc5 ultralow-frequency (ULF) waves, whether they can modulate the energy of magnetospheric ions is still poorly...- publication PDF
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How many active regions are necessary to predict the solar dipole moment?
We test recent claims that the polar field at the end of Cycle 23 was weakened by a small number of large, abnormally oriented regions, and investigate what this means for solar...- publication PDF
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GISandbox: A science gateway for geospatial computing
Science gateways provide easy access to domain-specific tools and data. The field of Geographic Information Science and Systems (GIS) uses myriad tools and datasets, which...- publication PDF
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Estimates of past and future ozone trends from multimodel simulations using...
A novel additive model analysis of multimodel trends is presented. The approach is motivated by, and particularly suited to, the analysis of multimodel time series of varying...- publication PDF
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Atmospheric lunar tide in the low latitude thermosphere-ionosphere
We present simultaneous, independent measurements of the atmospheric semidiurnal lunar tide in neutral winds and plasma velocities from NASA's Ionospheric Connection Explorer,...- publication PDF
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Improvement of advanced microwave sounding unit tropical cyclone intensity...
Previous work, in which Advanced Microwave Sounding Unit (AMSU) data from the Atlantic Ocean and east Pacific Ocean basins during 1999-2001 were used to provide objective...- publication PDF
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Evidence of liquid dependent ice nucleation in high-latitude stratiform...
Ground-based lidar, radar and microwave radiometer observations at Eureka, Canada, Barrow, Alaska and over the western Arctic Ocean measure physical characteristics and...- publication PDF
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What controls the entrainment rate of dry buoyant thermals with varying...
This study uses theory and numerical simulations to analyze the nondimensional spreading rate a (change in radius with height) of buoyant thermals as they rise and entrain...- publication PDF
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An evaluation of WRF's ability to reproduce the surface wind over complex...
The performance of the Weather Research and Forecasting (WRF) model to reproduce the surface wind circulations over complex terrain is examined. The atmospheric evolution is...- publication PDF
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Propagation of biases in climate models from the synoptic to the regional...
Bias adjustment methods usually do not account for the origins of biases in climate models and instead perform empirical adjustments. Biases in the synoptic circulation are for...- publication PDF
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Vertical temperature profiles at maximum entropy production with a net...
Like any fluid heated from below, the atmosphere is subject to vertical instability that triggers convection. Convection occurs on small time and space scales, which makes it a...- publication PDF
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Robust but weak winter atmospheric circulation response to future Arctic sea ice loss
The possibility that Arctic sea ice loss weakens mid-latitude westerlies, promoting more severe cold winters, has sparked more than a decade of scientific debate, with apparent...- publication PDF
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Resolving temperature limitation on spring productivity in an evergreen...
The flow of carbon through terrestrial ecosystems and the response to climate are critical but highly uncertain processes in the global carbon cycle. However, with a rapidly...- publication PDF
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Roles of barotropic instability across the moat in inner eyewall decay and...
Intense tropical cyclones (TCs) often experience secondary eyewall formations and the ensuing eyewall replacement cycles. Better understanding of the underlying dynamics is...- publication PDF
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Evaluation of scalar advection schemes in the Advanced Research WRF model...
In the Advanced Research Weather Research and Forecasting Model (ARW), versions 3.0 and earlier, advection of scalars was performed using the RungeâKutta time-integration...- publication PDF
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Regional soil moisture biases and their influence on WRF model temperature...
Operational Weather Research and Forecasting (WRF) Model forecasts run over Dugway Proving Ground (DPG) in northwest Utah, produced by the U.S. Army Test and Evaluation Command...- publication PDF
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Climatology and pre-convection environmental conditions of dry and wet...
Thunderstorm high wind (THW) is defined as a kind of convective weather phenomenon with a maximum wind gust speed not less than 17.2 m·sâ1 over China. It is a sudden,...- publication PDF
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Performance of the HOMME dynamical core in the aqua-planet configuration of...
A new atmospheric dynamical core, named the High Order Method Modeling Environment (HOMME), has been recently included in the NCAR-Community Climate System Model version 4...- publication PDF
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A statistical estimate of errors in the calculation of radio-occultation...
Atmospheric data from National Centers for Environmental Prediction (NCEP) analyses and orbital parameters from 133 real Global Positioning System (GPS) meteorological data...- publication PDF