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Evaluation of three temperature profiles of a sublayer scheme to simulate...
The diurnal cycle of sea surface temperature (SST) plays an important role in the upper ocean and climate system. One way to represents the diurnal variation of SST in Ocean...- publication PDF
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Evaluation and improvements of two community models in simulating dry...
Dry deposition velocities (V-d) for peroxyacetyl nitrate (PAN) calculated using two community dry deposition models with different treatments of both stomatal and nonstomatal...- publication PDF
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Description and derived climatologies of automated in situ...
The statistical properties of turbulence at upper levels in the atmosphere [upper troposphere and lower stratosphere (UTLS)] are still not well known, partly because of the lack...- publication PDF
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Distance-dependent filtering of background error covariance estimates in an...
The usefulness of a distance-dependent reduction of background error covariance estimates in an ensemble Kalman filter is demonstrated. Covariances are reduced by performing an...- publication PDF
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The potential impact of nuclear conflict on ocean acidification
We demonstrate that the global cooling resulting from a range of nuclear conflict scenarios would temporarily increase the pH in the surface ocean by up to 0.06 units over a...- publication PDF
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Stochastic decadal projections of Colorado River streamflow and reservoir...
Decadal (similar to 10-year)-scale flow projections in the Colorado River Basin (CRB) are increasingly important for water resources management and planning of its reservoir...- publication PDF
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Skill assessment of HF radar-derived products for Lagrangian simulations in...
Since January 2009, two long-range high-frequency (HF) radar systems have been collecting hourly high-spatial-resolution surface current data in the southeastern corner of the...- publication PDF
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HESS Opinions "A perspective on isotope versus non-isotope approaches to...
Current techniques to disentangle the evaporative fluxes from the continental surface into a contribution evaporated from soils and canopy, or transpired by plants, are under...- publication PDF
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Magnetosphere-ionosphere coupling via prescribed field-aligned current...
The magnetosphere-ionosphere (MI) coupling is crucial in modeling the thermosphere-ionosphere (TI) response to geomagnetic activity. In general circulation models (GCMs) the MI...- publication PDF
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The multi-scale aerosol-climate model PNNL-MMF: Model description and evaluation
Anthropogenic aerosol effects on climate produce one of the largest uncertainties in estimates of radiative forcing of past and future climate change. Much of this uncertainty...- publication PDF
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Probing into the impact of 3DVAR assimilation of surface PM₁₀ observations...
The capability of assimilating surface PM₁₀ (particulate matter with diameters less than 10 µm) observations has been developed within the National Centers for Environmental...- publication PDF
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Mitigation of 21st century Antarctic sea ice loss by stratospheric ozone recovery
We investigate the effect of stratospheric ozone recovery on Antarctic sea ice in the next half-century, by comparing two ensembles of integrations of the Whole Atmosphere...- publication PDF
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Evaluation of humidity correction methods for Vaisala RS92 tropical sounding data
This study examines the DigiCORA and Global Climate Observing System Reference Upper-Air Network (GRUAN) humidity corrections of Vaisala RS92 radiosondes at three sites over the...- publication PDF
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Future changes in coastal upwelling ecosystems with global warming: The case...
Coastal upwelling ecosystems are among the most productive ecosystems in the world, meaning that their response to climate change is of critical importance. Our understanding of...- publication PDF
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Measurements of light-absorbing particles on the glaciers in the Cordillera...
Glaciers in the tropical Andes have been rapidly losing mass since the 1970s. In addition to the documented increase in temperature, increases in light-absorbing particles...- publication PDF
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Evaluation of forecasted southeast Pacific stratocumulus in the NCAR, GFDL,...
Forecasts of southeast Pacific stratocumulus at 20°S and 85°W during the East Pacific Investigation of Climate (EPIC) cruise of October 2001 are examined with the ECMWF model,...- publication PDF
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Combining artificial intelligence with physics-based methods for...
A modern renewable energy forecasting system blends physical models with artificial intelligence to aid in system operation and grid integration. This paper describes such a...- publication PDF
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Seasonal differences in the response of Arctic cyclones to climate change in CESM1
The dramatic warming of the Arctic over the last three decades has reduced both the thickness and extent of sea ice, opening opportunities for business in diverse sectors and...- publication PDF
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Climates of the 20th and 21st centuries simluated by the NCAR Climate System Model
The Climate System Model, a coupled global climate model without "flux adjustments" recently developed at the National Center for Atmospheric Research, was used to simulate the...- publication PDF
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Estimating the meridional extent of adiabatic mixing in the stratosphere...
Wave-induced adiabatic mixing in the winter midlatitudes is one of the key processes impacting stratospheric transport. Understanding its strength and structure is vital to...- publication PDF
