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International Centre for Earth Simulation
The Symbiosis of Science, Society and Nature
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ABOUT
ICES
Biennial Workshop VI
Biennial Workshop V
- Workshop interviews
Biennial Workshop IV
Building an open, integrated holistic model of Planet Earth
'Asia in a Changing Monsoon' symposium
ICES 2017 RISK Award
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EARTH SCIENCES
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THE BIOSPHERE
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SPECIFIC EVENTS:
Three Mile Island 1979
Chernobyl 1986
Aceh Tsunami 2004
Hurricane Katrina '05
Wenchuan Quake '08
Haiti Earthquake 2010
Chilean Earthquake '10
Queensland Floods '10
Great East Japan 2011 Earthquake & Tsunami
Fukushima Meltdown
Thailand floods 2011
Superstorm Sandy '12
Cyclone Phailin 2013
Typhoon Haiyan 2013
MH370 Disappears '14
Nepal Earthquake '15
Tianjin Explosion 2015
Ecuador Quake 2016
SierraLeoneMudslide'17
Hurricane Harvey 2017
Hurricane Irma 2017
Hurricane Maria 2017
Santa Rosa Fire 2017
Thomas Fire 2017
El Fuego eruption '18
Hurricane Florence '18
AnakKrakatau tnmi '18
Whaley Bridge dam '19
Australian bushfires 2019-20
Beirut explosion 2020
Texas Big Freeze 2021
Tonga eruption 2022
PATH TO INTEGRATION
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COMPUTING
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OUTREACH
Science as Art
FACILITY
Main Aspects of Earth's Structure & Dynamics
Earth Science Literacy Principles
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Solid Earth:
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Paleo-Earth
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Earth's Spin Axis & Rotation
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Milankovitch Cycles
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Earth's Core, Mantle, Crust, Continents, Ocean Basins, Plumes & Plate Tectonics
The solid Earth is made up from multiple layers - each layer exhibiting its own set of characteristics and physical processes: the Inner Core, Outer Core, Mantle, Crust, Continents & Ocean Basins. Our understanding of the interaction between these layers is however, embryonic.
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Subduction
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Mountain Ranges: Himalayas, Rockies, Andes, Alps, Atlas
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Volcanoes
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Ring of Fire
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Earthquakes & Seismic Waves
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The Critical Zone
The Critical Zone (CZ) is a dynamic region where rock, soil, water, air, and living biota interact to shape Earth’s surface. The Critical Zone ranges from the tops of the trees to the bottom of groundwater. The field of hydrogeophysics employs geophysical methods to determine parameters and monitor processes associated with water resources, the water cycle, and contaminant transport to inform hydrogeological studies. All of CZ science could benefit from the temporal and spatial information provided by hydrogeophysics; however, to date the two fields have evolved largely in parallel.
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Landscape formations
The land and soil beneath our feet has been either laid down, built up, or exuded over millions of years. The mapping and naming of its main formations, and a description of the processes involved is covered by the articles below:
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Soil Science
Soil is the bridge between geology and biology
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Science of Rocks
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Nature's Magnificent Crystals
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Impact Craters
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Arid Lands & Deserts
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Salt Flats
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Grasslands & Meadows
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Lakes, Rivers, Deltas and Groundwater
Water exists in many forms and plays a multitude of different roles in the on-going evolution of the planet. The totality of all water is known as the hydrosphere. Hydrology is the science of water.
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Aquifers
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Wetlands, Peatlands & Marshes
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The Oceans:
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Coastal Zones
Where land meets water there are a multitude of dynamics that carve out unique and interesting features, all of which enrich the complexity of Earth's surface structure. The never ending impact of water on rock and sand creates a complex dynamic, rich in special phenomena.
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Oceans & Seas
The oceans cover more than 70% of the Earth's surface. They are critical to all life, and differentiate the Earth from most other planets in the known universe. The oceans are connected by a continuous flowing circulation current which plays a major role in driving Earth's climate.
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Ocean Ridges & Rises
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Deap Sea Hydrothermal Vents & Methane Gas Craters
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Coral Reefs
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The Cryosphere:
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Dynamics of the Cryosphere
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Permafrost & Tundra
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The Arctic Region
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Greenland
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Iceland
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Antarctica
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The Atmosphere
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Structure & Dynamics of the Atmosphere
Atmospheric scientists study the atmosphere's physical characteristics, motions, and processes, and the way in which these factors affect the rest of our environment. Knowledge of the atmosphere, its chemistry, structure and behavior is becoming increasingly relevant to the development of a safe and secure society.
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Winds: Trade, Horse Latitudes, the Doldrums, other
Solar radiation warms the air over the equator, causing it to rise. The rising air then proceeds south and north toward the poles. From approximately 20° to 30° North and South latitude, the air sinks. Then, the air flows along the surface of the earth back toward the equator.
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Clouds & Contrails
Although clouds play an important role in the Earth's Water Cycle and in modulating the amount of radiation from the Sun striking the Earth's surface, much has yet to be discovered as to how clouds form and evolve, and precisely how they contribute to the Earth's weather and climate. Accurate cloud data is missing from most climate models.
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Lightning & Sprites
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Atmospheric electricity - Global Electric Circuit (GEC)
The GEC extends throughout Earth’s atmosphere, creating a potential drop of 200,000 to 500,000 volts between the ground and the ionosphere. The circuit courses through the atmosphere even on fair-weather days when a slight current of 2 picoamps (or 0.0000000000002 A) flows from every square meter of ground upward.
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Ozone Hole
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Weather Forecasting
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Earth's Thermosphere:
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Earth's Albedo (reflectance)
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Earth's Energy Budget
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Solar Irradiance
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Earth's Plasmasphere:
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The Ionosphere
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