The AMMA programme Results & new challenges from a WCRP perspective

Slides:



Advertisements
Similar presentations
2010 update of GCOS IP in support of UNFCCC Paul Mason and Stephan Bojinski GCOS Steering Committee September 2010.
Advertisements

WCRP polar climate predictability initiative Vladimir Ryabinin
Africa Group paper session, Monday 18 February 2008 Charlie Williams Climate modelling in AMMA Ruti, P. M., Hourding, F. & Cook, K. H. CLIVAR Exchanges,
Quantitative information on agriculture and water use Maurits Voogt Chief Competence Center.
Surface control on albedo and radiation balance over the Gourma site Laurent Kergoat, Olivier Samain, Françoise Guichard, Pierre Hiernaux, Franck Timouk,
4th Training Course on WMO SDS-WAS products: (satellite and ground observation and modelling of atmospheric dust) November 2014, Casablanca, Morocco.
Scaling Laws, Scale Invariance, and Climate Prediction
Potential Predictability and Extended Range Prediction of Monsoon ISO’s Prince K. Xavier Centre for Atmospheric and Oceanic Sciences Indian Institute of.
The Impact of Irrigation on Land-Atmosphere Interactions and Indian Monsoon Precipitation.
Coordinated Enhanced Observing Period (CEOP) an Element of WCRPinitiated by GEWEX EOP1: Jul.-Sep EOP3: Oct Sep
AMMA-UK WP3 – Convection and dynamics Doug Parker Institute for Atmospheric Science School of Earth and Environment University of Leeds 29 November 2004.
“Kick Off Meeting” Instituto Franco-Argentino sobre Estudios de Clima y sus Impactos. Institut Franco-Argentin sur le Climat et ses Impacts. Institut Franco-Argentin.
Observed characteristics of the mean Sahel rainy season This talk (1) The basic state (some conclusions from the JET2000 field campaign) (2) Mesoscale.
AMMA-UK Kick-off meeting Jan 2005 WP1 Land surface and atmosphere interactions Chris Taylor Phil Harris.
Section 3.4 Introduction to the West African Monsoon.
Coupling Strength between Soil Moisture and Precipitation Tunings and the Land-Surface Database Ecoclimap Experiment design: Two 10-member ensembles -
Outline Background, climatology & variability Role of snow in the global climate system Indicators of climate change Future projections & implications.
Impact of Sea Surface Temperature and Soil Moisture on Seasonal Rainfall Prediction over the Sahel Wassila M. Thiaw and Kingtse C. Mo Climate Prediction.
Challenges and Limitations of regional climate model simulations in West Africa for Present and Future studies Gregory S. Jenkins Penn State University.
© Crown copyright 03/2014 Met Office and the Met Office logo are registered trademarks Met Office FitzRoy Road, Exeter, Devon, EX1 3PB United Kingdom Tel:
© Crown copyright Met Office Climate Projections for West Africa Andrew Hartley, Met Office: PARCC national workshop on climate information and species.
South Eastern Latin America LA26: Impact of GC on coastal areas of the Rio de la Plata: Sea level rise and meteorological effects LA27: Building capacity.
CryosPheric responses to Anthropogenic PRessures in the HIndu Kush-Himalaya regions: impacts on water resources and society adaptation in Nepal DHM Centre.
Changes and Feedbacks of Land-use and Land-cover under Global Change Mingjie Shi Physical Climatology Course, 387H The University of Texas at Austin, Austin,
GHP and Extremes. GHP SCIENCE ISSUES 1995 How do water and energy processes operate over different land areas? Sub-Issues include: What is the relative.
West African Monsoon Modeling and Evaluation (WAMME) Project Yongkang Xue, Bill Lau, Kerry Cook With contributions from many collaborators C20C Workshop.
Continental Tropical Convergence Zone (CTCZ) Programme under the Indian Climate Research Programme (ICRP)
Surface energy (and water) budget in the Sahel during the multi-decadal drought: combining remote sensing and in situ data. Laurent Kergoat (CNRS/LMTG,
High resolution simulation of August 1 AMMA case: impact of soil moisture initial state on the PBL dynamics and comparison with observations. S. Bastin.
Variation of Surface Soil Moisture and its Implications Under Changing Climate Conditions 1.
Characterization of tropical convective systems Henri Laurent IRD/LTHE Cooperation with Brazil CTA (Centro Técnico Aeroespacial) CPTEC (Centro de Previsião.
CPPA Past/Ongoing Activities - Ocean-Atmosphere Interactions - Address systematic ocean-atmosphere model biases - Eastern Pacific Investigation of Climate.
Part I: Representation of the Effects of Sub- grid Scale Topography and Landuse on the Simulation of Surface Climate and Hydrology Part II: The Effects.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Analysis of surface meteorological data at the Gourma sites focus on radiative fluxes & thermodynamics at diurnal & interannual time scales automatic weather.
UNCLASS1 Dr. Gene Whitney Assistant Director for Environment Office of Science and Technology Policy Executive Office of the President WISP Meeting - July.
PROMISE Coordinator’s Summary of Year 2 Annual Report delivered on time (almost!) Cost statement still to be completed but expenditure and man months seem.
LASG/IAP Collaboration between CLIVAR/AAMP and GEWEX/MAHASRI A proposal to foster interaction l Coordinated GCM/RCM Process study on Monsoon ISO l Multi-RCM.
© Crown copyright Met Office Uncertainties in the Development of Climate Scenarios Climate Data Analysis for Crop Modelling workshop Kasetsart University,
Why the African Initiative needs a research component … and a suggested framework Mitch Moncrieff Cloud Systems Group NCAR/MMM African Initiative Workshop,
Dr. Monia Santini University of Tuscia and CMCC CMCC Annual Meeting
© Crown copyright Met Office Deep moist convection as a governor of the West African Monsoon 1 UK Met Office, 2 University of Leeds, 3 National Centre.
WCC-3, Geneva, 31 Aug-4 Sep 2009 Advancing Climate Prediction Science – Decadal Prediction Mojib Latif Leibniz Institute of Marine Sciences, Kiel University,
Methods of Detection of change and feedback in semi-arid regions (North Africa and Sahel) Chehbouni A. Ghani ; L. Jarlan and E. Mougin Center of Space.
DIAS INFORMATION DAY GLOBAL WATER RESOURCES AND ENVIRONMENTAL CHANGE Date: 09/07/2004 Research ideas by The Danish Institute of Agricultural Sciences (DIAS)
Response of Sahelian vegetation to climatic variability Consequences for the Surface-Atmosphere interactions Mougin E. 1, Hiernaux P. 1, Kergoat L. 1,
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Importance of the atmospheric boundary layer (2).
ESSL Holland, CCSM Workshop 0606 Predicting the Earth System Across Scales: Both Ways Summary:Rationale Approach and Current Focus Improved Simulation.
ENSEMBLES Workshop, Toulouse Feb. 9-10, Centre National de Recherches Météorologiques (CNRM-GAME / Météo-France, Toulouse)‏ 2 Centre d’Etudes Spatiales.
Institute for Climate and Atmospheric Science SCHOOL OF EARTH AND ENVIRONMENT Deep moist convection as a governor of the West African Monsoon C. E. Birch.
The Water Cycle - Kickoff by Kevin Trenberth -Wide Ranging Discussion -Vapor -Precip/Clouds -Surface Hydrology (Land and Ocean) -Observations and scales.
EC-PHORS GCW YOPP The WMO Global Cryosphere Watch (GCW) is an international mechanism for supporting all key cryospheric in-situ and remote sensing observations.
Years of the Maritime Continent ( )
Paleoclimate Models (Chapter 12).
17.1 Climate and its causes.
Global Impacts and Consequences of Climate Change
IGOS Cryosphere Theme The cryosphere is an integral part of the global climate system, modulating surface energy and moisture fluxes, clouds, precipitation,
Model Summary Fred Lauer
Investigations of Land-Atmosphere Interactions in the West African Monsoon using Satellite remote Sensing Phil Harris1, Chris Taylor1, Doug Parker2, Richard.
Session D6: Process Based Evaluation of the West African Monsoon in CORDEX Projections Goal: Assess components of the West African Monsoon that are both.
The AMMA project: Studying the climate and environment of West Africa
South Eastern Latin America
Oceanic Origin of the Precipitation Jump in the Sahel
Twentieth Century & Future Trends.
20th Century Sahel Rainfall Variability in IPCC Model Simulations and Future Projection Mingfang Ting With Yochanan Kushnir, Richard Seager, Cuihua Li,
Michel Rixen, WCRP Joint Planning Staff
SAWS-SERV-RES-WEATHERSMART-SYMPOSIUM-2019
Global Observational Network and Data Sharing
Biomass and Soil Moisture simulation and assimilation over Hungary
Presentation transcript:

The AMMA programme Results & new challenges from a WCRP perspective 4/27/2019 The AMMA programme Results & new challenges from a WCRP perspective Jean Luc Redelsperger, LPO & CNRM, France E. Afiesima, A. Diedhiou, S. Janicot, T. Lebel, D.J. Parker, C. Thorncroft (AMMA Executive Committee) 1

The largest regional deficit of rainfall observed during the last century Sahel rainfall index Wet period 20% 10% -10% -20% Dry Period

UNCERTAINTIES ABOUT THE FUTURE

Precip Jul-Aug-Sept: (2070-99) minus (1960-99) Last IPCC report, SRES A1b: Uncertainties on rain changes for future years Precip Jul-Aug-Sept: (2070-99) minus (1960-99) Decrease over Sahel Increase over Sahel

African Monsoon Multidisciplinary Analyses Afrikanske Monsun: Multidisiplinære Analyser Afrikaanse Moesson Multidisciplinaire Analyse Analisi Multidisciplinare per il Monsone Africano Afrikanischer Monsun: Multidisziplinäre Analysen Analisis Multidiciplinar de los Monzones Africanos Analyses Multidisciplinaires de la Mousson Africaine `

A coordinated international program on West African monsoon, its variability and society-environnement-ressources-climat Interactions Aim 1 To improve our understanding of the WAM & its influence on environment regionally & globally Aim 2 To provide the underpinning science -to relate WAM variability to related societal issues -to define & implement relevant monitoring & prediction strategies Aim 3 To ensure that the AMMA research is integrated with prediction & decision making activities (EWS) Phase 1: 2002-2009 Coordination : Multidisciplinary Research , Different communities International : ~600 people from 30 countries Africa : ~250 pers ; Research and Application (Forecast/EWS) communities Field experiments Long term multidisciplinary observation networks Modelling; Satellite Products tailored & validated Unique database with mirror in Africa (Obs, Models, Sat, Library) Training/Education: PhD (160 incl 80 Africans) Masters, Summer Schools, Workshops Communication (external & internal) AMMA coordinated with international programmes and bodies

Research field experiments A coordinated international program on West African monsoon, its variability and society-environnement-ressources-climat Interactions Aim 1 To improve our understanding of the WAM & its influence on environment regionally & globally Aim 2 To provide the underpinning science -to relate WAM variability to related societal issues -to define & implement relevant monitoring & prediction strategies Aim 3 To ensure that the AMMA research is integrated with prediction (weather to climate) & decision making activities (EWS) Research field experiments SOP 2006: - First international experiment in Africa at regional scale - A unique data set documenting simultaneously the sea-air-continent system over a full seasonal cycle and over an eco- climatic transect

A coordinated international program on West African monsoon, its variability and society-environnement-ressources-climat Interactions Aim 1 To improve our understanding of the WAM & its influence on environment regionally & globally Aim 2 To provide the underpinning science -to relate WAM variability to related societal issues -to define & implement relevant monitoring & prediction strategies Aim 3 To ensure that the AMMA research is integrated with prediction (weather to climate) & decision making activities (EWS) Field experiments SOP 2006: -First international experiment in Africa at regional scale - A unique data set documenting simultaneously the sea-air-continent system over a full seasonal cycle and over an eco- climatic transect EOP 2005-2007: 3 years of unprecedented monitoring of water, energy, aerosol cycles over land, ocean and atmosphere at the regional and mesoscale, coordinated with socio-economic observation strategies LOP 2002 – 2009: A long term monitoring program of key continental and oceanic regions

Multidisciplinary observatories on agriculture, vegetation, livestock and climate Agriculture surveys: 9 sites (from 450mm to 900mm per year), 2 to 10 villages per site, 3 crop types & many varieties Rangeland surveys: 3 transects (from 100mm to 1000mm per year), > 50 sites on various soils, vegetation types and pastoral pressure status 10

Restoring the West African radiosonde network necessary to make forecasts & to monitor climate July 2004 August 2006 Greatest density of atmospheric soundings ever launched with 21 active stations 200 radiosonde operators and technicians working on the network + students and researchers from Africa, the Americas and Europe

AMMA Radiosoundings: A Major Achievement of AMMA

Example: Weather & climate forecast to advice the agricultural sector Red : Date of first rainfall over Sahel Blue: Date of cold water formation in Gulf of Guinea Equatorial region of gradients of surface flux (Ocean towards Atmosphere) To forecast the beginning of the rainy season (monsoon onset) To better advice for first seeding in Sahel => See poster of Thorncroft Session xx

ALMIP illustration Africa maps

Annual cycle of sensible heat flux (Mean 2005-2007) 60 X 60 km2 : 3 AMMA-CATCH stations in Mali Aggregated (green aera : spread) ; ALMIP LSM average +/- stabdard deviation(purple) The three-year average (2005-07) observed Qh for the three local sites are indicated by the non-filled symbols, and the shaded green area corresponds to the spread of the spatially aggregated fluxes (representing the 60x60 km2 meoscale domain). The solid purple curves enclose a region bounded by +/- one standard deviation about the ALMIP LSM average Qh averaged over 2005-07. Note that Exp. 3 results are used here since they extend to 2007. The observed flux data for this figure were taken from Timouk et al. (2009). ISBA It is hard to say in detail...but when we do the local scale runs for ALMIP2, we hope to get a better idea of "why"...but we can say already: Most of the models used (in some way) ECOCLIMAP, so the albedo and emissivity was nearly the same among the models...along with the same imposed forcing, so Rnet is probably NOT a big contributor to model discrepancy. This then likely points to an over-estimated Evap after the rainy season. (It could be a vegetation-roughness or z0h/z0m issue since the z0 changes after the rainy season) It could be related to other aspects too of course (soil moisture uptake, etc...) but again, I'll look more closely at the local scale.. Figure from Boone, A. et al , BAMS 2009 ; Observations from Timouk et al J Hydrol 2009

Global Global SST Teleconnections Remote effects of MJO 10 4 km Regional Scales Interactions Monsoon Systems Major River Basins 10 3 km Mesoscale Mesoscale Convective Systems Intraseasonal scale is a central scale fro the understanding of Monsoon variability and its impacts 10 2 km Catchments Vegetation Soil Deep Conv Cells Pools Vegetation Soil Local Shallow Cells 10 1 km Hour Day Season Year Diurnal Cycle Seasonal Cycle Interannual Variability

Atmospheric boundary layer feedback to soil moisture anomalies Wind & surface temperature spectrally coherent down to λ~20km PBL & surface temperature spectrally coherent down to λ ~ 20km Surface-induced temperature gradients induce wind convergence

Surface rain & Energy budget: Observations & AMIP Simulations Sahel 15°N Cumulative rainfall Surface net radiation OBSERVATIONS (Black curve) Major problems in models, even before the monsoon onset & the rain Multiples possible reasons : Surface representation but also aerosols & clouds + 7 modèles simulations avec SST prescrite Traoré, Guichard, Hourdin PRECIPITATIONS & BILAN ENERGETIQUE A LA SURFACE

First picture of the West Africa atmospheric composition Airborne measurements Average CO concentrations through out troposphere (>50hPa) based on 1-min data from the Bae-146, DLR Falcon, French Falcon 20th July-21 AUgust

First tests to improve NWP products & EWS AMMA Phase 1 (2002-2009) Aim 1 To improve our understanding of the WAM & its influence on environment regionally & globally Aim 2 To provide the underpinning science -to relate WAM variability to related societal issues -to define & implement relevant monitoring & prediction strategies Aim 3 To ensure that the AMMA research is integrated with prediction & decision making activities (EWS) First tests to improve NWP products & EWS Process knowledge Multi-scale & multi-disciplinary with emphasis on geophysics part Building the scientific ground basis & a community to work on societal-climate issues

Scale Integration (up/down) & Pluri-disciplinary AMMA Phase 2 (2010-2020) Aim 1 To improve our understanding of the WAM & its influence on environment regionally & globally Aim 2 To provide the underpinning science -to relate WAM variability to related societal issues -to define & implement relevant monitoring & prediction strategies Aim 3 To ensure that the AMMA research is integrated with prediction & decision making activities (EWS) International Science Plan 2 (2010-2020) (http://www.amma-international.org) Research Themes: (i) Interactions, Society, Climate (ii) Weather, Seasonal and Climate Predictability and Prediction (iii) Monsoon System Observations, Capacity Building & training, Coordination and scientific diffusion To move from understanding of system processes toward the one of process system (WAM) To pull-through of knowledge to improve prediction of weather & climate variability and associated societal impacts (New/Improved Climat & Weather Models; EWS ; tailored products) Scale Integration (up/down) & Pluri-disciplinary   Interactions Societies-Environment-Climate Relevant monitoring for Application & Research in regard societal-climate issues

AMMA has been very successful in its first phase: Improved understanding of the WAM in particular Establishment of observational network Built an international community in partnership with Africans Implemented important and crucial capacity building activities AMMA Phase 2 has great challenges: Pull-through of knowledge to improve prediction of weather and climate variability and associated societal impacts Maintain monitoring observation network Maintain strong coordination providing benefits from the go-to community for issues related to climate variability & climate change in the West African region linkages between science and applications for the benefit of society Partnership between numerous isolated projects sharing AMMA aims and benefiting AMMA (community, knowledge, database, …) Promote and strengthen AMMA-African leadership Lessons learned – to benefit the whole of Africa.