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Estimating parameters in a sea ice model using an ensemble Kalman filter
Uncertain or inaccurate parameters in sea ice models influence seasonal predictions and climate change projections in terms of both mean and trend. We explore the feasibility...- publication PDF
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Quantification of the SF6 lifetime based on mesospheric loss measured in the...
Sulfur hexafluoride (SF6) is a greenhouse gas with one of the highest radiative efficiencies in the atmosphere as well as an important indicator of transport time scales in the...- publication PDF
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Dynamical and microphysical evolution during mixed-phase cloud glaciation...
A bulk microphysics scheme predicting ice particle habit evolution has been implemented in the Weather Research and Forecasting Model. Large-eddy simulations are analyzed to...- publication PDF
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Summer high-wind events and phytoplankton productivity in the Arctic Ocean
At the base of the marine food web, phytoplankton are an essential component of the Arctic Ocean ecosystem and carbon cycle. Especially after sea ice retreats and light becomes...- publication PDF
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Estimation of X-band polarimetric radar attenuation and measurement...
A variational algorithm for estimating measurement error covariance and the attenuation of X-band polarimetric radar measurements is described. It concurrently uses both the...- publication PDF
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Assessing and improving the NWS point-and-click webpage forecast information
The National Weather Service (NWS) is the governmental agency responsible for providing freely available weather forecasts, warnings, watches, and advisories for the protection...- publication PDF
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Ensemble spread behavior in coupled climate models: Insights from the Energy...
Assessing uncertainty in future climate projections requires understanding both internal climate variability and external forcing. For this reason, single-model initial...- publication PDF
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Was the 2015 North Atlantic subpolar cold anomaly predictable?
The subpolar North Atlantic (SPNA) experienced extreme cold during 2015, an event often called the "cold blob." The evolution of this event in the Community Earth System Model...- publication PDF
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Divergent eddy heat fluxes in the Kuroshio Extension at 144°-148°E. Part I:...
The Kuroshio Extension System Study (KESS) provided 16 months of observations to quantify eddy heat flux (EHF) from a mesoscale-resolving array of current- and pressure-equipped...- publication PDF
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Carbonaceous matter in the atmosphere and glaciers of the Himalayas and the...
Carbonaceous matter, including organic carbon (OC) and black carbon (BC), is an important climate forcing agent and contributes to glacier retreat in the Himalayas and the...- publication PDF
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On the occurrence of the third-order scaling in high-latitude solar wind
This article does not have an abstract or article summary.- publication PDF
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Ecological processes dominate the ¹³C land disequilibrium in a Rocky...
Fossil fuel combustion has increased atmospheric CO₂ by ~ 115 µmol mol-1 since 1750 and decreased its carbon isotope composition (δ¹³C) by 1.7-2‰ (the ¹³C Suess effect). Because...- 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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Finescale structure of a snowstorm over the northeastern United States: A...
The newly developed High-Performance Instrumented Airborne Platform for Environmental Research (HIAPER) Cloud Radar (HCR) is an airborne, W-band, dual-polarization, Doppler...- publication PDF
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Global variability in atmospheric new particle formation mechanisms
A key challenge in aerosol pollution studies and climate change assessment is to understand how atmospheric aerosol particles are initially formed 1,2 . Although new particle...- publication PDF
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Kinetic-scale magnetic holes inside foreshock transients
In Earth's foreshock, there are many foreshock transients that have core regions with low field strength, low density, high temperature, and bulk velocity variation. Through...- publication PDF
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The Craig-Sneyd analytic solutions to the Parker problem
This paper follows up on the conclusion by Craig and Sneyd (2005) that the solutions to a linearized magnetostatic problem are counterexamples to the magnetostatic model of...- publication PDF
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Surface-atmosphere decoupling limits accumulation at Summit, Greenland
Despite rapid melting in the coastal regions of the Greenland Ice Sheet, a significant area (~40%) of the ice sheet rarely experiences surface melting. In these regions, the...- publication PDF
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The NOx dependence of bromine chemistry in the Arctic atmospheric boundary layer
Arctic boundary layer nitrogen oxides (NOx = NO2 + NO) are naturally produced in and released from the sunlit snowpack and range between 10 to 100 pptv in the remote background...- publication PDF
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Tropospheric Ozone Assessment Report: Tropospheric ozone from 1877 to 2016,...
From the earliest observations of ozone in the lower atmosphere in the 19th century, both measurement methods and the portion of the globe observed have evolved and changed....- publication PDF