Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section,...

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Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy

Transcript of Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section,...

Page 1: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Global annual cycle

F Kucharski

Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy

Page 2: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

http://www.windows2universe.org/earth/climate/cli_seasons.html

Page 3: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.
Page 4: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

External forcing

Longitude average ofSolar surface radiationIn W/m^2

This clearly drivesour seasons

Page 5: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Of course, this translates Into seasonal variations of surface temperature(here in degrees C)

However, note that the north-south excursions are much smaller……..and there is a 1-2 month shift -> Inertia of Oceans

Page 6: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

May be a more interestingfield: Sea-level pressure(shown here in hPa)

As you know, it rainswhere the pressure is low…

Page 7: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

But first have a look At the consequencesFor the zonal mean Winds [m/s].

Trades

Interesting interruptionsof trades: Monsoons!

Extratropical westerlies

Page 8: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

And finally precipitation:

The extratropical rainbelts

The tropical ITCZ

(precip in mm/day)

Page 9: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Diff temp djf-jja

Cool, why?

Page 10: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Even the global men surface temperature has a seasonal cycle(due to heat capacity differences between ocean and land)

Page 11: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Diff slp djf-jja

MediterranianClimates

Subtropicalmonsoons

Page 12: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

MediterranianClimates

Subtropicalmonsoons

Diff prec djf-jja

Page 13: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Picture can be quite different if we zoom into specific regions: Indian Monsoon

Page 14: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Seasonality of Indian Monsoon

Page 15: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Mechanism 2 : Different heat capacity of land and sea (land-sea breeze)

Page 16: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Mechanism 2 : Different heat capacity of land and sea (land-sea breeze)

Page 17: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Zoom into Mediterranean

Page 18: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Surface pressure: Azores high moving northwards

Page 19: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Zoom into the Mediterranean

Page 20: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

Also Carbon Dioxide has a seasonal Cycle……..

Page 21: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.
Page 22: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

SUMMARY

•The annual cycle is the largest climate variation on Earth.• It is forced by the Earth axis tilt with respect to the rotation axis around the sun.•The surface temperature reacts to this forcing with some delay, depending on the total heat capacity (land/ocean). •The responses of other climatic fields, such as surface pressure, winds and rainfall, is also very clear, but more complicated.•Usually the annual cycle is stronger in high latitudes than in low latitudes, particularly for temperature.•The climate in the mediterranean region is strongly influenced by the seasonal cycle, but also the climate in monsoon regions (i.e. Indian Monsoon).

Page 23: Global annual cycle F Kucharski Fred Kucharski, Abdus Salam ICTP, Earth System Physics Section, Climate Variability Group, Trieste, Italy.

THANK YOU!