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CLIVAR’s Variability of the American Monsoon Systems Panel (VAMOS). 2001: “VAMOS is based on two internationally coordinated monsoon experiments: MESA in South America and NAME in North America.”.

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Clivar s variability of the american monsoon systems panel vamos
CLIVAR’s Variability of the American Monsoon Systems Panel (VAMOS)

2001: “VAMOS is based on two internationally coordinated monsoon experiments: MESA in South America and NAME in North America.”

2009: The term "monsoon system" encompasses not only the summer monsoon rainfall in the tropical Americas, but also the perturbations in the planetary, synoptic and mesoscale flow patterns that occur in association with it, including those in the winter hemisphere.

The region of interest covers both the tropical and the extratropical Americas and surrounding oceans.


IASCLIP

Variability of the American Monsoon Systems (VAMOS)

The annual cycle of convection over the Americas

Horel et al. (1989)


VAMOS (2009)

Four Complementary Science Programs

• North American Monsoon Experiment (NAME)

• Monsoon Experiment for South America (MESA)

• VAMOS Ocean Cloud Atmosphere Land Study (VOCALS)

• Inter-Americas Study of Climate Processes (IASCLIP)

  • CLIVAR and GEWEX endorsed activity:

    • La Plata Basin Regional Hydroclimate Project

  • Cross-cuts:

    • Modeling

    • Extremes

    • Anthropogenic Climate Change

    • Decadal Predictability


  • The north american monsoon experiment
    The North American Monsoon Experiment

    Outstanding Questions and Remaining Challenges:

    Predictions:

    • Clear lack of predictability of many large-scale modes for long-lead pred.

    • Need for improved downscaling methods for improved short-lead seasonal and medium range predictions

    • Resolve the failure of free running coupled OAGCMs to realistically represent key features of the NAM hydroclimate

    • Develop a process-based consensus on climate change impacts on NAM

    D. Gochis, May 13, 2009


    Monsoon Experiment in South America (MESA)

    Chair: J. Marengo

    HYPOTHESIS:

    The SAMS provides a physical basis for

    determining the degree of predictability

    on short- and long timescales over the region.

    • Selected MESA  deliverables:

    • More comprehensive understanding of South American climate variability and predictability;

    • Strengthened multinational scientific collaboration;

    • Improved observing system design for monitoring and predicting the South American monsoon system;

    • Measurably improved weather and climate models that predict South American monsoon variability. 


    VAMOS Ocean Cloud Atmosphere Land Study

    (VOCALS)

    GOALS of VOCALS Improved understanding and regional/global model representation of aerosol indirect effects over the Southeast Pacific Climate System.

    Elimination of CGCM systematic errors in the SEP, and improved model simulations of the coupled system in the region and global impacts of its variability.www.eol.ucar.edu/projects/vocals

    23 Universities

    20 Research Institutions

    6 Operational centers


    www.eol.ucar.edu/projects/vocals

    • The VOCALS Regional Experiment (REx) off the Chilean Coast was completed in Oct-Nov 2008

    • A four-part report with Rex information put in VOCALS web site (www.eol.ucar.edu/projects/vocals )

    • Second VOCALS Meeting: 12-14 July 2009, Seattle, Washington

    • Data analysis and modeling continues in several centers.


    IASCLIP main science issues

    • What are the sources and predictability of summertime anomalies in the WHWP?

    • What are the structure and dynamics of the regional atmospheric circulation and low-level jets?

    • How does this flow depend on and interact with boundary conditions such as the WHWP, land heating, and topography to modulate precipitation and storms?

    • Within this climate setting, how can predictions of important weather phenomena such as tropical cyclogenesis events within the region be improved?

    IASCLIP Links

    IASCLIP–NAME

    Great Plains Precipitation

    IASCLIP-VOCALS

    Boreal summer circulation

    IASCLIP-MESA

    Boreal winter circulation

    5 largest warm pools

    5 smallest warm pools


    La Plata Basin research networks

    Multiple Regional Projects

    CLARIS - LPBA Europe-South America Network for Climate Change Assessment and Impact Studies

    IAI - LPB

    Ecosystems, Biodiversity,

    Land Use and Cover, and

    Water Resources


    CLARIS LPBhttp://www.claris-eu.org/

    - 10 countries, 20 institutions -

    Subproject 2: Past and future hydroclimate

    Subproject 4: Socio-economic scenarios and adaptation/ prevention strategies

    Courtesy of Anna Sorensson

    · WP3: Improving our description of recent past climate variability in La Plata Basin

    · WP4: Hydroclimate past and future low-frequency variability, trends and shifts

    · WP5: Regional Climate Change assessments for La Plata Basin

    · WP6: Processes and future evolution of extreme climate events in La Plata Basin

    · WP8: Land use change, agriculture and socio-economic implications

    · WP9: Water resources in La Plata Basin in the context of climate change


    Cross-cut:

    The VAMOS Modeling Plan

    http://www.clivar.org/organization/vamos/

    Publications/Vamos_Modeling_Plan_Jun08.pdf

    Ben Kirtman, Celeste Saulo and others


    Objectives

    Improve the prediction of warm season precipitation over the Americas, for societal benefit, and to assess the implications of climate change.

    The VAMOS modeling plan seeks improvements to how we model the interactions between the local processes and regional and larger scale variability in regional and global models.

    Model development efforts must take on a multi-scale approach that integrates across all of the[science programs in VAMOSand, on the global scale, link with the wider modeling initiatives in CLIVAR and WCRP.


    VAMOS modeling plan

    http://www.clivar.org/organization/vamos/

    Publications/Vamos_Modeling_Plan_Jun08.pdf

    • Introduction

    • 2.Modeling Strategy: A Multi-Scale Approach

    • 3. Representation of monsoon processes for improving prediction

    • A) Simulating, Understanding and Predicting the Diurnal Cycle

    • B) Predicting the Pan-American Monsoon Onset, Mature and Demise Stages

    • C) Modeling and Predicting SST Variability in the Pan-American Seas

    • D) Improving the Prediction of Droughts and Floods

    • 4.Data assimilation, Analysis and Assessing Observing Systems

    • 5.Prediction and Global-scale Linkages


    Prediction issues

    –Role of SSTs (especially other than ENSO)

    –Role of land surface feedbacks (strength, time scales)

    –Role of intraseasonal variability (e.g. MJO)

    –Seasonal and Decadal differences in predictability

    –Current Level of Quality


    VAMOS Extremes Task Force

    co-chaired by Lisa Goddard and Jean-Philippe Boulanger (2008/9)*

    *2009-- Siegfried Schubert and Iracema Cavalcanti (TBC)

    VAMOS will consider its continental perspective in linking extremes in warm season climate behavior to the circulation structures defined as the monsoon systems.

    The VAMOS Extremes Task Force considered:

    (1) Issues that are coherent across VAMOS program areas,

    (2) Aspects of extremes that can be somewhat unique to VAMOS, and

    (3) How to capitalize and complement existing and on-going efforts within the climate community (e.g., USCLIVAR; CEOP).

    (4) Social impact of extremes: seeking to quantify the cost of specific extreme events

    http://www.clivar.org/organization/vamos/Publications/vamos_extremes_21jul08.pdf


    VAMOS Anthropogenic Climate Change task force

    Tereza Cavazos, Dave Gochis, J.-P. Boulanger, J. Marengo

    nn

    In the climate change context, there is a need to identify and understand important processes that control monsoonal climates in the Americas, their variability and changes, and how these processes interact withbroader societal issues, such as impacts, vulnerability and adaptation.

    • Challenges

  • Assessment of GCM model performance and uncertainties

  • Improvement of the simulation and understanding of major

  • tropical and monsoon-related modes of variability

  • Investigation of the role of aerosols, land cover and land

  • use on the radiative balance and hydrological processes

  • Development of detection and attribution studies

  • Regional climate downscaling for integrated assessments

  • of climate change


  • Regional impact assessment studies

    • Basic Needs

      • Observations of sufficient detail and scope are required to improve validation, models and model ensembles and to ensure that monsoon-related processes can be adequately elucidated, predicted and projected

      • Improve or create regional databases that include observations, GCM model simulations, and regional downscaling simulations at daily and monthly timescales of the American monsoon regions


    North american regional climate change assessment program narccap
    North American Regional Climate Change Assessment Program (NARCCAP)

    • Assess regional climate change for North Americaby downscaling 4 AOGCMs with 6 RCMs.

      • Each RCM downscales two AOGCMs

      • Standard output format similar to AR4/CMIP3, downloadable from the Earth System Grid (ESG).

    • Project phases and status:

      • Phase I: RCMs driven by reanalysis (1979-2004) to examine uncertainty in RCMs (completed)

      • Phase IIa: RCMs driven by AOGCM output for 20th century (1971-2000) (nearing completion)

      • Phase IIb: RCMs driven by AOGCM output from SRES A2 scenario (2041-2070) (nearing completion)


    MRCC (NARCCAP)

    U. Quebec,

    Ouranos

    RegCM3

    UC Santa

    Cruz, ICTP

    HadRM3

    Hadley

    Centre

    RSM

    Scripps

    WRF

    NCAR/

    PNNL

    MM5

    Iowa State

    NARCCAP Design

    Current climate or Scenario

    global climate models

    CGCM3

    HadCM3

    CCSM

    GFDL

    Provide boundary conditions

    regional climate models


    CLARIS-LPB (NARCCAP)

    Regional climate change assessments

    WP5 specific objectives:

    ● Coordinate efforts to produce ensembles of the regional models toward an integrated view of the expected regional hydroclimate in South America in general and La Plata Basin in particular.

    ● Investigate the range of differences between the projections employing a suite of mesoscale regional models.

    ● Contribute to the knowledge of downscaled climate model scenarios for the La Plata basin region, and quantify their associated uncertainties.


    CLARIS-LPB WP-5 (NARCCAP)

    Regional climate change and downscaling

    - Regional climate model scenarios (BCs: A1B)

    1990-2005 (ERA-Interim), GCMs

    2010-2040

    2070-2100

    - Metrics

    Specific deliverables are:

    5.1: A set of metrics to be employed in model performance

    5.2: Uncertainties in simulations from Task 1 will be examined and reported.


    Selected CLIVAR Priorities (NARCCAP)

    • Anthropogenic Climate Change

    • Natural variability versus forced change

    • Climate sensitivity and feedbacks

    • Regional phenomena

    • Extremes

    • Decadal Variability, Predictability and Prediction

    • Intra-to-Seasonal Variability, Predictability and Prediction

    • Monsoons (and ENSO, TAV, …)

    • ISV/MJO


    • Analysis and Evaluation

    • “Climate Process Teams” (process studies)

    • Capacity Building

    • Summer schools

    • Topical workshops

    • Expert training


    In summary: (NARCCAP)

    VAMOS can contribute with its regional expertise to advance CLIVAR’s Imperatives…

    VAMOS promotes communications between science components, Cross-cuts, Research networks…

    VAMOS is interested in increasing and strengthening the links with USCLIVAR and other Climate Programs…

    Thanks…


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