1 / 12

Towards Passive Microwave Radiance Assimilation of Clouds and Precipitation

Towards Passive Microwave Radiance Assimilation of Clouds and Precipitation Ralf Bennartz 1 , Tom Greenwald 2 , Andrew Heidinger 3 , Chris O’Dell 1 , Martin Stengel 1 , Kenneth Campana 4 , Peter Bauer 5 1: Atmos. & Oceanic Sci. ,University of Wisconsin 2: CIMSS ,University of Wisconsin

Download Presentation

Towards Passive Microwave Radiance Assimilation of Clouds and Precipitation

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Towards Passive Microwave Radiance Assimilation of Clouds and Precipitation Ralf Bennartz1, Tom Greenwald2, Andrew Heidinger3, Chris O’Dell1,Martin Stengel1, Kenneth Campana4, Peter Bauer5 1: Atmos. & Oceanic Sci.,University of Wisconsin 2: CIMSS,University of Wisconsin 3: NOAA/NESDIS 4: NOAA/NCEP 5: ECMWF

  2. Outline • SOI model and applications • Cloud/precipitation overlap • 3-year accomplishments • Further plans

  3. SOI Radiative Transfer Model • Hybrid multi-stream solution method (doubling plus iteration) (Heidinger et al. 2006; O’Dell et al. 2006) • Implementation - Less scattering: 2-stream solution - More scattering: 4-stream solution • Forward, tangent linear and adjoint models integrated into CRTM

  4. Accuracy of Results (Eddington and SOI versus Monte-Carlo model)

  5. Forward and adjoint simulation example GFS Simulations AMSR-EObservations

  6. Infrared Applications: MSG SEVIRI

  7. MSG SEVIRI Comparison Results

  8. Different cloud/precipitation overlap models • Conventional approach uses cloud cover to subdivide NWP pixel in cloudy/precipitation • New approach derives two or three optimal columns based on subscale distribution of precipitation columns with similar optical properties • Numerically efficient (2-3 radiative transfer calculations per NWP grid point) • Highly accurate against independent column/Max-Random-overlap reference • Optimal approach reduces errors due to cloud overlap from maximum values of 5-10 K to values < 1K

  9. Different cloud/precipitation overlap models 1Column 2Columns 3columns 3 optimal Currently operational at ECMWF O’Dell, Bauer, Bennartz, JAS, 2006, submitted

  10. Different cloud/precipitation overlap models 1Column 2Columns 3columns 3 optimal New scheme with much better error characteristics Currently operational at ECMWF O’Dell, Bauer, Bennartz, JAS, 2006, submitted

  11. 3-year Accomplishments • Fast forward RT model (SOI) developed, tested and integrated in CRTM (3 publications) • Tangent linear and adjoint model developed, tested, and integrated in CRTM • Bias GFS/SOI statistics for passive microwave and infrared • Fast and accurate new cloud overlap scheme for use in NWP radiance assimilation (forward/adjoint); manuscript submitted

  12. Further plans • Monitor bias statistics over longer time period, especially: • Fully include scattering (need more complete GFS input data) • Biases in IR including scattering • Precipitation assimilation: • Include cloud diagnostics to generate precipitation rate • Further test and integrate cloud overlap with NCEP/GFS.

More Related