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Climate responses to the splitting of a supercontinent: Implications for the...
Reconstructing deep time climate often relies on a limited number of data points, which can hinder inference of the large‐scale climate state. Here we use an Earth system model...- publication PDF
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An advanced scheme for wet scavenging and liquid-phase chemistry in a...
Clouds are reaction chambers for atmospheric trace gases and aerosols, and the associated precipitation is a major sink for atmospheric constituents. The regional chemistry-...- publication PDF
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Reply to comments on "Multiyear predictions of North Atlantic hurricane...
This article does not have an abstract or article summary.- publication PDF
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Reconstruction of global monthly upper-level temperature and geopotential...
This work presents statistically reconstructed global monthly mean fields of temperature and geopotential height (GPH) up to 100 hPa for the period 1880–1957. For the...- publication PDF
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IGS ROTI Maps: Current status and its extension towards equatorial region...
The International GNSS Service (IGS) diurnal ROTI maps ionospheric product was developed to characterize ionospheric irregularities occurrence over the Northern hemisphere and...- publication PDF
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Using CCSM3 for paleoclimate applications
This document describes the procedures for creating a CCSM3 paleoclimate simulation in the fully coupled (all active components) configuration. We provide tools and examples of...- publication PDF
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Day‐to‐day variability of prereversal enhancement in the vertical ion drift...
Equatorial plasma bubbles (EPBs) are plasma density irregularities found in the equatorial ionosphere after sunset and are closely related to the upward ExB drift before it...- publication PDF
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Representing subgrid convective initiation in the Community Earth System Model
A widely recognized issue found in most Earth System Models is that of convective precipitation being triggered too early during the day over land, often resulting in persistent...- publication PDF
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Case Studies on Convective Storms / Case Study 4, 27 July 1976: First Echo Case
On 27 July 1976, a relatively small, weak storm was investigated by the NCAR/NOAA instrumented sailplane in coordination with NCAR Queen Air 306D. The potential instability was...- publication PDF
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Effect of different emission inventories on modeled ozone and carbon...
In order to improve our understanding of air quality in Southeast Asia, the anthropogenic emissions inventory must be well represented. In this work, we apply different...- publication PDF
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The genesis of Typhoon Nuri as observed during the Tropical Cyclone...
Aircraft reconnaissance data collected during the Tropical Cyclone Structure 2008 field campaign are used to examine further kinematical, dynamical, and thermodynamical aspects...- publication PDF
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Development of a method to detect high ice water content environments using...
This paper describes development of a method for discriminating high ice water content (HIWC) conditions that can disrupt jet-engine performance in commuter and large transport...- publication PDF
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Global soil carbon projections are improved by modelling microbial processes
Society relies on Earth system models (ESMs) to project future climate and carbon (C) cycle feedbacks. However, the soil C response to climate change is highly uncertain in...- publication PDF
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Intercomparisons of HIRDLS, COSMIC and SABER for the detection of...
Colocated temperature profiles from the Constellation Observing System for Meteorology, Ionosphere and Climate (COSMIC), High Resolution Dynamics Limb Sounder (HIRDLS) and the...- publication PDF
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The White Light Solar Corona: An Atlas of 1985 K-coronameter Synoptic Charts...
This article does not have an abstract or article summary.- publication PDF
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Transition and equilibration of neutral atmospheric boundary layer flow in...
The Weather Research and Forecasting Model permits finescale large-eddy simulations (LES) to be nested within coarser simulations, an approach that can generate more accurate...- publication PDF
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A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: Sea ice data...
The Last Interglacial period (LIG) is a period with increased summer insolation at high northern latitudes, which results in strong changes in the terrestrial and marine...- publication PDF
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Numerical modeling of the large-scale neutral and plasma responses to the...
We study the response of the thermosphere and ionosphere to gravity waves (GWs) excited by 6 h of deep convection in Brazil on the evening of 01 October 2005 via the use of...- publication PDF
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The equatorial El Niño-Southern Oscillation Signatures observed by...
This paper uses the tropospheric pressure, temperature, and water vapor pressure observed by six micro-satellites of the FORMOSAT-3/COSMIC (F3/C) constellation to study El Niño-...- publication PDF
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Medium-scale gravity wave activity in the bottomside F region in tropical regions
Thermospheric gravity waves (GWs) in the bottomside F region have been proposed to play a key role in the generation of equatorial plasma bubbles (EPBs). However, direct...- publication PDF