Jordmassa

Jorden fotograferad av NASA.

Jordmassa (M🜨) är en måttenhet som motsvarar jordens massa, 1 M🜨 = 5,9742 × 1024 kg. Måttet jordmassa används ofta inom populärvetenskapen för att beskriva massor hos stenplaneter.

De fyra stenplaneterna i solsystemet: Merkurius, Venus, jorden och Mars, har massor på 0,055, 0,915, 1,000 respektive 0,107 jordmassor.

En jordmassa kan omvandlas till liknande enheter:

Referenser

Den här artikeln är helt eller delvis baserad på material från engelskspråkiga Wikipedia, Earth mass, tidigare version.
  1. ^ Williams, Dr. David R. (2 november 2007). ”Jupiter Fact Sheet”. NASA. Arkiverad från originalet den 5 oktober 2011. https://www.webcitation.org/62D9vKbZz?url=http://nssdc.gsfc.nasa.gov/planetary/factsheet/jupiterfact.html. Läst 16 juli 2009. 

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This spectacular “blue marble” image is the most detailed true-color image of the entire Earth to date. Using a collection of satellite-based observations, scientists and visualizers stitched together months of observations of the land surface, oceans, sea ice, and clouds into a seamless, true-color mosaic of every square kilometer (.386 square mile) of our planet. These images are freely available to educators, scientists, museums, and the public. This record includes preview images and links to full resolution versions up to 21,600 pixels across.


Much of the information contained in this image came from a single remote-sensing device-NASA’s Moderate Resolution Imaging Spectroradiometer, or MODIS. Flying over 700 km above the Earth onboard the Terra satellite, MODIS provides an integrated tool for observing a variety of terrestrial, oceanic, and atmospheric features of the Earth. The land and coastal ocean portions of these images are based on surface observations collected from June through September 2001 and combined, or composited, every eight days to compensate for clouds that might block the sensor’s view of the surface on any single day. Two different types of ocean data were used in these images: shallow water true color data, and global ocean color (or chlorophyll) data. Topographic shading is based on the GTOPO 30 elevation dataset compiled by the U.S. Geological Survey’s EROS Data Center. MODIS observations of polar sea ice were combined with observations of Antarctica made by the National Oceanic and Atmospheric Administration’s AVHRR sensor—the Advanced Very High Resolution Radiometer. The cloud image is a composite of two days of imagery collected in visible light wavelengths and a third day of thermal infra-red imagery over the poles. Global city lights, derived from 9 months of observations from the Defense Meteorological Satellite Program, are superimposed on a darkened land surface map.