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PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from...

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Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific climate simulated by CCSR/NIES/FRCGC coupled models PICES XV (2006) in Yokohama PICES XV (2006) in Yokohama
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Page 1: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

Hiroyasu HASUMI (CCSR)Takashi SAKAMOTO (FRCGC)

and many more from CCSR/NIES/FRCGC

Overview of present state and future projection of North Pacific climate simulated by CCSR/NIES/FRCGC coupled models

PICES XV (2006) in YokohamaPICES XV (2006) in Yokohama

Page 2: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

Japan KJapan K--1 Project Team1 Project TeamResearch consortium of

-Center for Climate System Research (CCSR), the University of Tokyo

-National Institute for Environmental Studies (NIES)

-Frontier Research Center for Global Change (FRCGC)

has contributed to the IPCC AR4

Two models of different resolution→ What does resolution matter in climate projection? (with a focus on the North Pacific)

Page 3: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

Coupled GCMCoupled GCM

High Medium

Atmosphere: CCSR/NIES/FRCGC AGCM 5.7

T106 (~1.1°)56 levels

T42 (~2.8°)20 levels

Ocean: CCSR OceanComponent Model 3.4

~0.28°x0.19°47 levels

~1.4°x0.5°-1.4°43 levels

Land: MATSIRO ~0.56° ~2.8°

River: TRIP 0.5° ~2.8°

Sea ice: dynamic (EVP)-thermodynamic (0-layer)

same as ocean same as ocean

MIROC (Model for Interdisciplinary Research On Climate) version 3.2

Page 4: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

Coupled GCMCoupled GCMBiases in annual-mean SST of the control (pre-industrial condition) runs

High-resolution

Medium-resolution

Page 5: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

ExperimentsExperiments

High and Medium Medium only

2020thth CenturyCentury

1850/1900 2000 2100 2200 2300

Scenario RunsScenario Runs(Coupled(Coupled))

Year Year 20002000 FixFix

A1BA1BB1B1

A1B Year A1B Year 21002100 FixFixA2A2

ControlControl

B1 Year B1 Year 21002100 Fix Fix

0 70 140 220 290

1%/yr CO1%/yr CO22 Incr.Incr.(Coupled)(Coupled)

4xCO4xCO22 FixFix

COCO 22Increase 1%/year

Increase 1%/year

SpinSpin--upup

100 150

2xCO2xCO22 FixFixControlControl

Runs for IPCC AR4 and CMIP Coordinated Ex.

Page 6: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

LargeLarge--scale feature of global warmingscale feature of global warmingSAT and rain: (2071-2100 of A1B) - (1971-2000)

Page 7: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?

SAT/SLP/V850June (control)Obs.

High-res. Med-res.

Baiu/Meiyu front

Page 8: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?Daily rainfall frequency over Japan(120E-140E, 30N-40N)

Page 9: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?

Summertime mean rainfall

Number of days of heavy (> 100 mm/day) rainfall

Change of rainfall over Japan by high-res. model

Page 10: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?Annual-mean 100 m velocity

High-resolution

Medium-resolution

Page 11: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?Kuroshio: (2071-2100 of A1B) – (1971-2000)

Sakamoto et al. (2005)

+30 cm/s

Page 12: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?Curl τ change: (2071-2100 of A1B) – (1971-2000)

Sakamoto et al. (2005)

-Acceleration of the Kuroshio accounted for by Sverdrup transport ~5 Sv

-Actual acceleration ~30 Sv

Page 13: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?Wind change: (2071-2100 of A1B) – (1971-2000)

Sakamoto et al. (2005)

-Weakened trades-Intensified Aleutian Low… El Nino-like response (Many models project El Nino-like SST rise under global warming)

Page 14: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

What does resolution matter?What does resolution matter?Coupled effect of resolution dependence?

- Higher resolution AGCM → better atmosphere (Baiu/Meiyu front, tropical cyclone, …)

- Higher resolution OGCM → bettern ocean (Kuroshio, eddy and variability, …)

- Does atmospheric (oceanic) resolution affect ocean (atmosphere)?

- Is there any air-sea feedback affecting resolution dependence?

What is improved by resolution? How and why?

Page 15: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

CrossCross--bred modelsbred modelsControl climate simulations by models with different combinations of resolution- T106(1°) AGCM + 1/4°x1/6° OGCM

high-AGCM high-OGCM → hAhO- T42(3°) AGCM + 1° OGCM

medium-AGCM medium-OGCM → mAmO- T106 AGCM + 1° OGCM

high-AGCM medium-OGCM → hAmO- T42 AGCM + 1/4°x1/6° OGCM

medium-AGCM high-OGCM → mAhO- T213(0.5°) AGCM + 1/4°x1/6° OGCM

super-high-AGCM high-OGCM → sAhO

Page 16: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

CrossCross--bred modelsbred modelsKuroshio axis for high-OGCM cases(16°C contours at 200 m depth)

sAhOhAhOmAhO

Page 17: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

[m/s]

CrossCross--bred modelsbred modelsAtmospheric resolution and the Oyashio (subpolargyre)

hAhO mAmO

hAmO mAhO

Page 18: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

[hPa]

CrossCross--bred modelsbred modelsWintertime sea level pressure

Stronger Aleutian Low ←?→ Stronger Oyashio

hAhO mAmO

hAmO mAhO

Page 19: PICES XV (2006) in Yokohama · Hiroyasu HASUMI (CCSR) Takashi SAKAMOTO (FRCGC) and many more from CCSR/NIES/FRCGC Overview of present state and future projection of North Pacific

SummarySummary- Question: What is improved by resolution in

climate simulations and projections?How and Why?

- Running models of various combination of atmospheric and oceanic resolution… Ongoing work


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