Intercomparison of methods of coupling between convection and large‐scale circulation: 2. Comparison over nonuniform surface conditions-Reference-Cited by-同舟云学术

Intercomparison of methods of coupling between convection and large‐scale circulation: 2. Comparison over nonuniform surface conditions

Published:2016-03 Issue:1 Volume:8 Page:387-405
ISSN:1942-2466
Container-title:Journal of Advances in Modeling Earth Systems
language:en
Short-container-title:J. Adv. Model. Earth Syst.

Author:

Daleu C. L.¹,Plant R. S.¹,Woolnough S. J.²,Sessions S.³,Herman M. J.³,Sobel A.⁴,Wang S.⁵,Kim D.⁶,Cheng A.⁷,Bellon G.⁸,Peyrille P.⁹,Ferry F.⁹,Siebesma P.¹⁰¹¹,van Ulft L.¹⁰

Affiliation:

1. Department of MeteorologyUniversity of ReadingReading UK

2. National Centre for Atmospheric ScienceDepartment of Meteorology, University of ReadingReading UK

3. Department of PhysicsNew Mexico TechSocorro New Mexico USA

4. Department of Environmental SciencesColumbia UniversityNew York New York USA

5. Department of Applied Physics and Applied MathematicsColumbia UniversityNew York New York USA

6. Department of Atmospheric SciencesUniversity of WashingtonSeattle Washington USA

7. Climate Science Branch, NASA Langley Research CentreHampton Virginia USA

8. The Department of PhysicsUniversity of AucklandAuckland New Zealand

9. Meteo FranceToulouse France

10. Royal Netherlands Meteorological InstituteDe Bilt Netherlands

11. Delft University of TechnologyDelft Netherlands

Funder

NERC

the NCAS, a NERC collaborative center

U.S. National Science Foundation

NSF

the NASA

DOE Atmospheric System Research Program under Interagency agreements

the European Commission's Seventh Framework Programme

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015MS000570

Reference41 articles.

1. Relationships between Water Vapor Path and Precipitation over the Tropical Oceans

2. Simulation of shallow cumuli and their transition to deep convective clouds by cloud-resolving models with different third-order turbulence closures

3. Cloud-Resolving Model Simulations with One- and Two-Way Couplings via the Weak Temperature Gradient Approximation

4. Transition from Suppressed to Active Convection Modulated by a Weak Temperature Gradient–Derived Large-Scale Circulation

5. Intercomparison of methods of coupling between convection and large-scale circulation: 1. Comparison over uniform surface conditions

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