Download presentation

Presentation is loading. Please wait.

Published byAmber Montgomery Modified over 3 years ago

1
Robin Hogan and Jon Shonk Implementation of multiple regions in Edwards-Slingo

2
Shadows! Need separate regions even in clear skies? Downward short-wave flux (W m -2 )Upward short-wave flux (W m -2 ) Natural logarithm of IWC (g m -3 )

3
Anomalous horizontal transport Homogenization of clear-sky fluxes: –Reflected radiation has more chance to be absorbed -> TOA shortwave bias –Effect is very small in the longwave This problem can be solved in a way that makes the code more efficient Single cloud

4
Two-stream scheme F 1.5 + F 1.5 - F 0.5 + F 0.5 - F 2.5 + F 2.5 - Consider a two- layer atmosphere Solve a tridiagonal matrix problem to obtain the fluxes Layer 1 reflection, transmission and emission: R 1, T 1, S 1 +, S 1 - Layer 2 reflection, transmission and emission: R 2, T 2, S 2 +, S 2 - TOA flux: S TOA - Surface emission and albedo: S s +, s

5
It is conceptually convenient to solve the system by –Working up from the surface calculating the albedo i and upward emission G i of the whole atmosphere below half-level i. –Then working down from TOA, calculating the upwelling and downwelling fluxes from i and G i. Edwards-Slingo solution

6
Two-regions: cloud and clear-sky a a b b Layer 1 Layer 2 With 2 regions (a & b), matrix is denser –Latest Edwards-Slingo only has approximate solvers SOLVER_MIX_DIRECT and SOLVER_TRIPLE for the 3-region version –OK for upright convection but unacceptable errors introduced with realistic overlap Note that the overlap coefficients have been omitted in this example

7
New version a a b b Layer 1 Layer 2 But some elements represent unwanted anomalous horizontal photon transport –Remove them and the problem can be solved exactly, and in closer agreement with ICA –Enables triple (and quadruple, quintuple…) regions to be implemented quite easily! R ab R ab is the reflection from region a to region b at the same level

8
Performance of new solver In calculating upwelling flux at half-level 1.5, downwelling flux sees albedo of whole atmosphere below, 1.5, which it reflects back into the same region –Much closer to the independent column approximation! 0.5 1.5

Similar presentations

OK

METO 621 Lesson 12. Prototype problems in Radiative Transfer Theory We will now study a number of standard radiative transfer problems. Each problem assumes.

METO 621 Lesson 12. Prototype problems in Radiative Transfer Theory We will now study a number of standard radiative transfer problems. Each problem assumes.

© 2017 SlidePlayer.com Inc.

All rights reserved.

Ads by Google

Ppt on needle stick injury Ppt on airbag working principle of motor Ppt on boilers operations management Ppt on natural resources and conservation degrees Ppt on op amp circuits filter Ppt on samsung galaxy note 2 Ppt on online shopping project Ppt on zener diode current Ppt on mobile tv seminar Pledge to the bible ppt on how to treat