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NAME Modeling and Data Assimilation

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Title: NAME Modeling and Data Assimilation


1
NAME Modeling and Data Assimilation White
PaperJune 2003
       
 
  • Provides a strategy for accelerating progress
    on the fundamental modeling issues pertaining to
    the NAME science objectives
  • Unveiled at NAME Modeling and Data
    Assimilation Workshop (UMD, June 03)
  • Reviewed by the US CLIVAR Pan American Panel.
  • Emphasizes activities that bring
    observationalists, modelers and physical
    parameterization experts together to focus on key
    physical processes that are deficient in coupled
    models.


NAME Modeling and Data Assimilation
A Strategic Overview
NAME Science Working Group
June 2003
 
2
IMPROVE warm season prediction
  • Improve understanding and prediction of the life
    cycle of the North American monsoon system and
    its variability.
  • warm season convective processes in complex
    terrain (Tier 1)
  • intraseasonal variability of the monsoon(Tier 2)
  • the response of warm season atmospheric
    circulation and precipitation patterns to slowly
    varying, potentially predictable oceanic and
    continental surface conditions (Tier 3)

3
Strategy
  • I. Multi-scale Model Development
  • II. Multi-tier Synthesis and Data Assimilation
  • III. Prediction and Global-scale Linkages

4
GUIDING PRINCIPALS The strategy must take
maximum advantage of NAME enhanced observations,
and should simultaneously provide model-based
guidance to the evolving multi-tiered NAME
observing program. The modeling activities must
maintain a multi-scale approach in which local
processes are embedded in, and are fully coupled
with, larger-scale dynamics.
5
NAMAPModel Assessment for the North American
Monsoon Experiment
  • D.S. Gutzler H.-K. Kim
  • University of New Mexico NOAA/NCEP/CPC
  • gutzler_at_unm.edu hyun-kyung.kim_at_noaa.gov

Thanks to CPC for hosting DGs visit, Spring
2003 NAMAP modeling participants UCAR/JOSS for
archiving NAMAP output
6
NAMAP Accomplishments
  • Establish the baseline simulations/forecasts
  • To know what we do not know
  • Position and structure of the GCLLJ
  • Diurnal cycle of the GCLLJ
  • Detailed structure and distribution
  • of rainfall (both in space and time)
  • d) Oceanic influencelocal and remote

7
  • No obs here! What is the true diurnal cycle?
  • All models show convective max between 21Z-04Z
  • Different diurnal max over different places

8
use the NAME data
  • Understand the dynamical processes related
  • to NAME
  • Better monitoring of the monsoon systems
  • and the warm season precipitation regimes over
    North and Central America
  • Verify model forecasts
  • Improve modeling the physical processes
  • related to the NAME
  • Improve the operational forecasts and applications

9
I. Multi-scale Model Development
Premise of the NAME modeling strategy is that
deficiencies in our ability to model "local"
processes are among the leading factors limiting
forecast skill in the NAME region.
Requires

-improvements to the physical
parameterizations
-improvements to how we model interactions
between local processes and the larger scales
10
I. Multi-scale Model Development
  • NAME Focus Tier I
  • moist convection in the presence of complex
    terrain
  • Diurnal cycle
  • land/atmosphere ocean atmosphere interactions
    in the presence of complex terrain
  • We will have the NAME data as guide

11
Bottom-up approaches
  • Multi-scale modeling -gt
  • M. Moncrieff

Cloud-system-resolving models having
computational domain(s) large enough to represent
interaction/feedback with large
scales Multiscale models explicitly represent
convective cloud systems
12
Computational domains
Cloud-resolving domain ( )
M. Moncrieff
13
top-down approaches
2. Global/regional models S. Schubert et al.
G. Zhang
  • Use the observations to determine
  • Resolution
  • test the current parameterizations in the
    presence of complex terrain, and larger-scale
    organization
  • E. g. Different convection schemes
  • Radiation-cloud interaction

14
II. Multi-tier Synthesis and Data Assimilation
Data assimilation is critical to enhancing the
value and extending the impact of the Tier I
observations
The specific objectives are
To better understand and simulate the various
components of the NAM and their interactions with
the larger-scales
To quantify the impact of the NAME observations
To identify model errors and attribute them to
the underlying model deficiencies
15
Regional CDAS (R-CDAS) and NAME Data Impact and
Prediction Experiments
Kingtse Mo and Wayne Higgins CPC/NCEP, Fedor
Mesinger--- UCAR/EMC,Hugo Berbery--- University
of Maryland
  • Real time monitoring of hydro-meteorological
    conditions during NAME 2004 based on regional
    reanalysis and RCDAS
  • Data impact studies
  • With data into the GTS system , data assimilation
  • will be done using CDAS (T62), GDAS( GFS
    T256) and R_CDAS relatively quickly
  • b) Same as (a) but without data from NAME
  • c) After 12 to 18 months, all data are collected
    including rain gauges, a final sets of data
    assimilation will be done using GDAS and RCDAS
  • d) forecasts (1-90 days) every 6h using GFS
    T126

16
All PIs, please help us
  • Please give me a list of
  • A) station WMO ID
  • B) lat-lon position
  • C) Data type and time
  • For all data entering the GTS network before
  • the cutoff time h16Z
  • Thanks

17
An Assessment and Analysis of the Warm Season
Diurnal Cycle over the Continental US/N. Mexico
in Global AGCMS Siegfried Schubert, Max Suarez,
Myong-In Lee -NASA/GSFC Isaac
Held-GFDL

Arun Kumar, Hyun-Kyung Kim, Wayne Higgins
NCEP/CPC
  • OBJECTIVES
  • 1) Assess / analyze the diurnal cycle in three
    different AGCMs
  • (NASA, NCEP and GFDL),
  • 2) Improve understanding of the important
    physical processes that drive
  • the diurnal cycle,
  • 3) Provide guidance for the development of
    physical parameterizations
  • aimed at improving the simulation of the warm
    season hydrological cycle
  • over the US / N. Mexico

http//janus.gsfc.nasa.gov/milee/diurnal
18
III. Prediction and Global-Scale Linkages
  • Once we have a reliable model we are able to
  • determine the predictability and prediction skill
    over the NAMS region associated with the leading
    patterns of climate variability
  • Extend to examine the precipitation regimes over
    North and Central America
  • determine the predictability and prediction
    skill associated with anomalous land surface
    conditions in the NAME region (e.g. soil
    moisture)
  • assess the relative influences of local and
    remote SSTs

19
Predictability and Forecast Skill In Global Models
Jae-Kyung E. Schemm et al. CPC/NCEP/NWS/NOAA
  • Objectives
  • 1) To examine the predictability of warm
    season precipitation over
  • the NAM region
  • 2) To quantify error growth due to model
    errors versus that due to
  • uncertainties in analyses and boundary
    conditions
  • 3) To assess the value of NAME observations
    for prediction
  • 4) To help define field campaigns to follow NAME
    2004.
  • Key Questions (ultimately critical for climate
    prediction)
  • How is the life cycle of the monsoon related to
    the evolution of oceanic and continental boundary
    conditions?
  • Can models reproduce the observed summertime
    precipitation in average years and years with
    strong SST influence?
  • Models
  • On board NSIPP, NCEP/GFS Possible GFDL,
    NCAR

20
Different stages of modeling
  • Regional model simulations
  • Convection, diurnal cycle, rainfall
    distribution
  • regional features
  • Observed SSTs Global forecasts-gt regional
  • Model nesting
  • Two tier prediction system
  • Predicted SSTs global model forecasts
  • Coupled model prediction

21
NAME DELIVERABLES
  • Observing system design for monitoring and
    predicting the North American monsoon system.
  • More comprehensive understanding of North
    American summer climate variability and
    predictability.
  • Strengthened multinational scientific
    collaboration across
  • Pan-America.
  • Measurably improved climate models that predict
    North American monsoon variability months to
    seasons in advance.

22
NAME ROADMAP
Pre-NAME 2004 Activities Diagnostics and
Analysis - Model (e.g. NAMAP Warm Season
Diurnal Cycle in AGCMs) - Reanalysis (global,
regional) NAME FOC Practice Forecasting
Workshops - NASA/CLIVAR Subseasonal Workshop /
NAME Modeling Workshop - NAME SWG-5 / NAME
Special Session (Puerto Vallarta) NAME 2004
Activities NAME EOP Forecaster Support -
Forecast Discussions / Operational Assessments
Real-time Monitoring, Analysis and Forecast
Products
23
NAME ROADMAP
Post-NAME 2004 Activities Model and Forecast
System Development - NAME CPT activities
(simulation of convective precipitation) -
Multi-scale modeling / CRM Experimental
Prediction - NAME 2004 case studies /
hindcasts - Sensitivity to SST and soil
moisture (operational centers) - Subseasonal
prediction (e.g. TISO.MJO) Diagnostics and
Analysis - Reanalysis (global, regional, NAME
data impact) - Model diagnostics (NAMAP 2)
Applications and Product Development -
Assessments (Hazards, North American drought
monitor) - Forecasts (North American seasonal
and subseasonal) - Applications (Agriculture,
Fire WX, Water Resource) Research and Dataset
Development - PACS-GAPP warm season
precipitation initiative
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