scholarly journals Supplementary material to "The aerosol-cyclone indirect effect in observations and high-resolution simulations"

2017 ◽  
Author(s):  
Daniel T. McCoy ◽  
Paul R. Field ◽  
Anja Schmidt ◽  
Daniel P. Grosvenor ◽  
Frida A.-M. Bender ◽  
...  
Keyword(s):  
High Resolution ◽  
Indirect Effect ◽  
Supplementary Material

scholarly journals The aerosol-cyclone indirect effect in observations and high-resolution simulations

2017 ◽  
Author(s):  
Daniel T. McCoy ◽  
Paul R. Field ◽  
Anja Schmidt ◽  
Daniel P. Grosvenor ◽  
Frida A.-M. Bender ◽  
...  
Keyword(s):  
High Resolution ◽  
Indirect Effect ◽  
Climate Models ◽  
Climate Model ◽  
Cloud Condensation Nuclei ◽  
Cloud Droplet ◽  
2014 Eruption ◽  
Cloud Droplet Number Concentration ◽  
Aerosol Cloud Interactions ◽  
First Time

Abstract. Aerosol-cloud interactions are a major source of uncertainty in predicting 21st century climate change. Using high-resolution, convection-permitting global simulations we predict that increased cloud condensation nuclei (CCN) interacting with midlatitude cyclones will increase their cloud droplet number concentration (CDNC), liquid water (CLWP), and albedo. For the first time this effect is shown with 13 years of satellite observations. Causality between enhanced CCN and enhanced cyclone liquid content is supported by the 2014 eruption of Holuhraun. The change in midlatitude cyclone albedo due to enhanced CCN in a surrogate climate model is around 70 % of the change in a high-resolution convection-permitting model, indicating that climate models may underestimate this indirect effect.

scholarly journals Supplementary material to "Evaluating High-Resolution Forecasts of Atmospheric CO and CO<sub>2</sub> from a Global Prediction System during KORUS-AQ Field Campaign"

2018 ◽  
Author(s):  
Wenfu Tang ◽  
Avelino F. Arellano ◽  
Joshua P. DiGangi ◽  
Yonghoon Choi ◽  
Glenn S. Diskin ◽  
...  
Keyword(s):  
High Resolution ◽  
Prediction System ◽  
Field Campaign ◽  
Supplementary Material

scholarly journals Supplementary material to "High-resolution quantification of atmospheric CO<sub>2</sub> mixing ratios in the Greater Toronto Area, Canada"

2017 ◽  
Author(s):  
Stephanie C. Pugliese ◽  
Jennifer G. Murphy ◽  
Felix R. Vogel ◽  
Michael D. Moran ◽  
Junhua Zhang ◽  
...  
Keyword(s):  
High Resolution ◽  
Mixing Ratios ◽  
Greater Toronto Area ◽  
Supplementary Material

scholarly journals Supplementary material to "Cloud feedbacks in extratropical cyclones: insight from long-term satellite data and high-resolution global simulations"

2018 ◽  
Author(s):  
Daniel T. McCoy ◽  
Paul R. Field ◽  
Gregory S. Elsaesser ◽  
Alejandro Bodas-Salcedo ◽  
Brian H. Kahn ◽  
...  
Keyword(s):  
High Resolution ◽  
Satellite Data ◽  
Extratropical Cyclones ◽  
Cloud Feedbacks ◽  
Supplementary Material

Supplementary material to "Effects of multi-temporal high-resolution remote sensing products on simulated hydrometeorological variables in a cultivated area (southwestern France)"

2017 ◽  
Author(s):  
Jordi Etchanchu ◽  
Vincent Rivalland ◽  
Simon Gascoin ◽  
Jérôme Cros ◽  
Aurore Brut ◽  
...  
Keyword(s):  
Remote Sensing ◽  
High Resolution ◽  
Multi Temporal ◽  
Supplementary Material

An Italian Flanged Dish from Gloucester

Britannia ◽  
2019 ◽  
Vol 50 ◽  
pp. 402-408
Author(s):  
Paul A. Tyers
Keyword(s):  
High Resolution ◽  
Resolution Image ◽  
Type Series ◽  
High Resolution Image ◽  
Supplementary Material ◽  
Italian Origin

ABSTRACTRecent re-examination of the pottery in the Gloucester Roman pottery type series has identified an unusual large flanged dish in a micaceous fabric from the tilery site at St Oswald's Priory, originally published in Britannia. Petrological analysis indicates that it is of Italian origin. There are currently only a handful of examples of this type known from outside Italy, and this is the first example securely identified from Britain. Supplementary Material, including a high-resolution image of the microphotograph of Gloucester TF214, is available online at https://doi.org/10.1017/S0068113X19000126.

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