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Jumping on Water wallpaper

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Original Size:1920x1200. Your device resolution:

Standard resolutions of Jumping on Water for mobile device

Aspect RatioResolutions
Mobile VGA240x320320x240640x480480x640
Mobile WVGA240x400480x800400x240800x480
Mobile iPhone320x480480x320640x960960x640
Mobile iPad1024x768768x1024
Tablet iPad 21024x1024
Tablet Android1280x1280
Mobile PSP480x272
Other Mobile208x176280x220288x160345x240384x234400x240416x352480x234480x272800x480

Standard resolutions of Jumping on Water for TV and video applications

Aspect RatioResolutions
4:3176x144352x288720x540768x576
16:9864x486960x7201024x5761280x7201366x7681280x10801440x10801440x10801920x1080
others720x480720x486720x5761440x1024

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ocean:

An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which occupies two-thirds of the planet's surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with "ocean" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land. Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of the Earth's surface. The ocean contains 97% of the Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.3 billion...

sea:

The sea, the world ocean, or simply the ocean, is the connected body of salty water that covers 70.8% of the Earth's surface. The sea moderates the Earth's climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been travelled and explored since prehistory, the modern scientific study of the sea—oceanography—dates broadly to the British Challenger expedition of the 1870s. The sea is conventionally divided into four or five large sections, such as the Pacific, called oceans while smaller sections, such as the Mediterranean, are known as seas. Owing to the present state of continental drift, the Northern Hemisphere is now fairly equally divided between land and sea (a ratio of about 2:3) but the South is overwhelmingly oceanic (1:4.7). Salinity in the open ocean is generally in a narrow band around 3.5% by mass, although this can vary in more landlocked waters, near the mouths of large rivers, or at great depths. About 85% of the solids

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