Title: Simulation of Present-Day Climate in the Caribbean using PRECIS RCM
1Simulation of Present-Day Climate in the
Caribbean using PRECIS RCM
M
Mr. Arnoldo Bezanilla Marlot
2SIMULATION OF THE PRESENT-DAY CLIMATE IN THE
CARIBBEAN USING PRECIS RCM.
Abel Centella Arnoldo Bezanilla Israel
Borrajero Daniel Martinez Institute of
Meteorology, Cuba
2
Climate Change Impacts on the Caribbean, UWI
Mona, Jamaica, June 15,17-2007
3SIMULATION OF THE PRESENT-DAY CLIMATE IN THE
CARIBBEAN USING PRECIS RCM.
Abel Centella Arnoldo Bezanilla Israel
Borrajero Daniel Martinez Institute of
Meteorology, Cuba
3
Climate Change Impacts on the Caribbean, UWI
Mona, Jamaica, June 15,17-2007
4OUTLINE OF PRESENTATION
- What is PRECIS?
- Simulating Present-Day Climate in the Caribbean
using PRECIS. - How well does PRECIS represent the Caribbean
Climate? - PRECIS and Tropical Cyclones. Preliminary results
- PRECIS-CARIBE Online Access to PRECIS Output
- What have we done, future plans.
- Summary
5Regional Climate Modeling (I)
The main goal of regional climate models
(RCMs) is to reproduce the main climatic features
in complex terrain, where mesoscale forcing
becomes important (Giorgi and Mearns, 1991) and
coarse-resolution global climate models (GCMs)
are not sufficient for assessing local climate
change (Aldrian et al. 2004).
6Regional Climate Modeling (II)
An example of a region where
present-generation GCMs are especially lacking in
their ability to represent complex terrain and
land-sea contrasts is the Caribbean zone. In this
region, tropical and extra-tropical systems
interact (Alfonso and Naranjo, 1996) and
frequently produce complex meteorological
conditions. The sea-breeze circulation in islands
and peninsulas favors the development of
convective systems (Riehl, 1979). In such a
complex meteorological situation, a
high-resolution model is necessary for meaningful
regional climate prediction
7PRECIS (Providing REgional Climates for Impact
Studies)
- A Regional Modelling System derived from Hadley
Centre GCM - Providing REgional Climates for Impact Studies
- PC-based regional climate model
- It can be set up and run over any area
- PRECIS is freely available
- It has two resolutions 25 km and 50 km
- PRECIS is a tool for dynamical downscaling
8Simulating Present-Day Climate in the Caribbean
using PRECIS
- Quasi-observed climate PRECIS forced by ECWRF
Reanalysis ERA15 (RCM ERA) - PRECIS driven by HadAM3 control run (RCM CTRL)
- Climate Research Unit database was used as
observed climate (CRU OBS) - RCM ERA and RCM CTRL are identical apart from
their driving data.
9How well does PRECIS represent the Caribbean
Climate?
- RCM ERA and RCM CTRL were compared with CRU OBS
- RCM ERA and RCM CTRL biases were also compared
- Temperature and Precipitation for land areas only
PRECIS land sea mask
10TEMPERATURERCM CTRL- CRU OBS
11PRECIPITATIONRCM CTRL- CRU OBS
12RCM CTRL- CRU OBSTemperature and Precipitation
seasonal cycle for Cuba
- Warm and dry biases are evident in RCM CTRL
simulation - Greater biases occur over Cuba and other islands
- The dry biases are more intense in summer
13TEMPERATURERCM ERA- CRU OBS
14PRECIPITATIONRCM ERA- CRU OBS
15RCM ERA- CRU OBSTemperature and Precipitation
seasonal cycle for Cuba
- Warm and dry biases also exist in RCM ERA
simulation - Greater biases occur over Cuba and other islands
- The dry biases are more intense in summer
16Partial conclusions
- There consistency beetwen CTRL and ERA biases
suggest the RCM model dont capture very well
some of the mesoscale process. - The significant summer dry biases observed in
both simulations motivate further analysis of
convective process. - Comparisons with GCM outputs are also needed to
assess the improvement that PRECIS could produce.
17The Frequency of tropical cyclones in the
Caribbean and Mexico as show in Regional Climate
Model simulations
- Cyclone representation is a potential tool for
- Investigate and assess the Model ability to
represent this type of event. - Investigate or project future TC behavior in the
area
18TCLVs detection methodology
- It is designed to work with daily mean fields
- On a grid of 0.44o (50 km), a point of minimum in
surface pressure is sought so that the averaged
pressure over a circumference of 6o (700 km)
centered in the point is at least 5.5 hPa greater
than in the point. - The difference between the maximum and minimum
values of the wind speed in a neighborhood of 3
grid points radius (1.3o or 150 km) centered in
the point of minimum pressure must be at least 40
km/h (11 m/s). - The end of the track of each individual vortex
occurs when in two consecutive days, the points
of two consecutive TCLV position are located at a
mutual distance of more than 7o (800 km). - The above criteria were adjusted in practice by
trial and error based on a detailed visual
analysis of selected animated image sequences in
the output of the model.
19S
E
W
N
20Historical North Atlantic and East-Central North
Pacific Tropical Cyclone Tracks, 1851-2005
National Oceanic and Atmospheric Administration,
Tropical Prediction Center/National Hurricane
Center
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24Partial conclusions
- The projected increase in temperature in Eastern
Pacific near the coast of Mexico and the smaller
increase projected for Western Tropical Atlantic
seem to be consistent with a greater projected
increase of TCLVs for Eastern pacific.
25The method allow us to identify possible change
in tropical cyclone activity, but
- More experiments are needed
- Add new fields to be used in the detection
criteria. - Specify the definition of TCLV based on daily
means of - surface parameters using the criteria defined
by - Walsh et al. for instant(hourly mean)
observations in a - limited run of the model.
- Adjust a theoretical Cyclone Model to obtain
hourly - values of main TCLV parameters from the mean
daily - fields.
- Validate the definition using the adjustment to
climatologic - data.
- Analyze the dependence of TCLVs on projected
- temperature and wind shear projections.
26PRECIS (Sharing Results)
http//precis.insmet.cu/Precis-Caribe.ht
m PRECIS-CARIBE Online Access to Climate
Change Scenarios in the Caribbean.
27PRECIS (Sharing Results)
28PRECIS (Outputs)
Two Kind of format for Data Download NetCDF y
ASCII
29PRECIS (Outputs)
Examples for small island countries
Grid results over Jamaica
Grid results over Haiti
30PRECIS (What have we Done)
As part of a very prominent collaborative
initiative between 5C, INSMET and UWI Jamaica and
Barbados
- 15 Years Reanalysis (1979-1993)
- 2 B1 30 Years Baseline Ensembles
- (Control Experiments) 1960-1990 (S)
- 3 A2 30 Years de future scenarios 2070-2100 (S).
- B2 30 Years de future scenarios 2070-2100 (S).
31PRECIS (At this moment upcoming work)
- ECHAM4 50km
- Control 1960-1990 31yrs
- A2 1990-2100 114 yrs
- B2 1990-2100 114 yrs
- ERA40 with sulphur cycle 50km
- Observed 1957-2002 45yrs
- SRES Control hourly with sulphur cycle 50km
- 1960-1969 10 yrs
- HadCM3 perturbed parameter ensemble members
(50km) - 1 High 1 Low 150 Years
32PRECIS (upcoming work)
- HadCM3 perturbed parameter ensemble members
(50km) - 1 High 1 Low 150 Years
33PRECIS (Possibilities)
- Obtain and Use our own scenarios for climate
change - To share the obtained results with all the
scientific community, and stakeholders. - The improvement of the Collaboration in the
Caribbean - Using the outputs to feed other numeric models
(Hydrological, Crops models, etc ) - The investigation of the extreme events in the
future (strength, duration, frequency, season
shifting, etc )
34PRECIS (Summary)
- Improvements on the Precis-Caribe Web Site,
Languages, outputs added for another scenarios
(HadCM3-B2) and another GCM (ECHAM4 A2 and B2
scenarios). - Define whether to make daily data available.
- Add some specific variables, another domain (high
res Scenario for West Indias). - Work more Deeply in the analysis and validation
of the outputs. ERA40 Data.
35Thanks !!!!
PRECIS Online Access http//precis.insmet.cu/Pre
cis-Caribe.htm Email precis.insmet_at_insmet.cu
Contacts PRECIS Group in Cuba Abel Centella
abel.centella_at_insmet.cu Arnoldo Bezanilla
arnoldo.bezanilla_at_insmet.cu Israel Borrajero
iborajero_at_met.inf.cu