1 / 7

CMIP5 : 2m correlation skill score

CMIP5 : 2m correlation skill score. Full Field. Detrended field. CNRM-CM5 Contribution to CMIP5 20 dates (1959, 1960, 1964, 1965 … 2004, 2005) 10 members for each date Pinatubo-like eruption in 2010 (10 members). Most of the skill is due to the trend

lowri
Télécharger la présentation

CMIP5 : 2m correlation skill score

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. CMIP5 : 2m correlation skill score Full Field Detrended field • CNRM-CM5 Contribution to CMIP5 • 20 dates (1959, 1960, 1964, • 1965 … 2004, 2005) • 10 members for each date • Pinatubo-like eruption in 2010 (10 members) • Most of the skill is due to the trend • Added value of the ocean initialization and high skill • The first year • In the North Atlantic Ocean + western Pacific • Poor skill in the central and eastern Pacific

  2. Beyond CMIP5 : work on ocean initialization • Ocean initialization :Nudging to the ECMWF ocean reanalysis NEMOVAR (ORCA1°) [1958 -2008] • Several tests have been performed to set the optimal parameters for surface and subsurface restoring GLOB No 3D nudging within the 1°S–1°N band EXTROP No 3D nudging Within the 15°S–15°N band

  3. Beyond CMIP5 : work on ocean initialization Yr1 Yr2 Yr3 Yr4 NINO34 SST Ensemble mean (dates+members) Nino34 SST index Perturbation of the tropical climate up to 4yr (systematic NINO the 1st and 3rd year) when subsurface are initialized in the tropics

  4. Beyond CMIP5: impact of the stratosphere LT • Low Top configuration • 61 vertical level (5 hPa) • T63 horizontal Grid Full Field • High Top configuration • 91 vertical level (0.01 hPa) with exact same levels as LT in the troposphere • T63 horizontal Grid HT • Experiments • 10 dates (1980, 1981, 1983, 1986, 1988, 1990, 1991, 1993, 1996, 2001) • 5 more to come (1989, 1995, 1998, 2000, 2003) • 6 members for each date • 5 years long Detrended field No significant changes compared to CMIP5 No significant added value when the stratosphere is well resolved

  5. Beyond CMIP5 : the 2006-2023 forecast • Model : CNRM-CM5 • Initialization : Same as CMIP5 • 3 series of 10 members for 2006-2021 forecast • Control ensemble (decadal): RCP4.5 forcing + solar • Fictitious Pinatubo-like eruption in 2010 (VolcIn2010) • Suppressed 11yr solar cycle (SolarMin : maintain to the 2009 record minimum over the forecast period) • + 1 series of 10 members for 2006-2021 RCP4.5 projection 2m-Temperature Global precip • Colder start when initialized in 2006 versus RCP4.5 • Warmer climate at the end of the forecast vs RCP4.5 • Fictitious Pinatubo significant effect up to 2016 • Minor global effect for SUN

  6. Volcanic forcing : regional features 2m-Temperature WINTER SUMMER MSLP 2m-Temperature 2m-Temperature MSLP Mean [2010-2014] difference between the fictitious Pinatubo exp. and the control decadal experiment

  7. Solar forcing : regional features 2m-Temperature WINTER SUMMER MSLP 2m-Temperature 2m-Temperature MSLP Mean [2011-2016] difference between the SolarMin exp. and the control decadal experiment

More Related