…the thermometer at a weather station in El Azizia, Libya, reached 58.0°C (136.4°F). That measurement shifted the title for “the world’s hottest place” away from Death Valley, California, which set the previous record (56.7°C or 134°F) in July 1913. However, more recent research says that neither location has a true claim to the title. “Most of the places that call themselves the hottest on Earth are not even serious contenders,” said Steve Running of the University of Montana. The images above show a portion of the Lut Desert in Iran. The left image is natural color, while the right is infrared; both were acquired on July 6, 1999, by Landsat 7. In a study of seven years of global land surface temperatures as measured by satellites, the Lut Desert ranked as hottest in five of the years.
NASA images by Jesse Allen and Robert Simmon, using Landsat 7 data from the USGS Global Visualization Viewer. Caption by Mike Carlowicz.
That’s where satellites come in. Orbiting instruments can scan every parcel of the planet’s surface and fill in the gaps in global temperature measurements. In their analysis, Running, Mildrexler, and Maosheng Zhao scrutinized global measurements of land “skin” temperatures from 2003 to 2009. As opposed to air temperatures, which are measured 1.5 to 2 meters above the ground, land skin temperatures reflect the pure heating of a parcel of ground by radiation from the sun, the atmosphere, and other heat flows.
In five of the seven years—2004, 2005, 2006, 2007, and 2009—the highest surface temperature on Earth was found in the Lut Desert. The single highest LST recorded in any year, in any region, occurred there in 2005, when MODIS recorded a temperature of 70.7°C (159.3°F)—more than 12°C (22°F) warmer than the official air temperature record from Libya.
The University of Montana team found that the location of the world’s hottest spot can change from year to year, though the conditions don’t. Think dry, rocky, and dark-colored lands. In the images above from the Lut Desert, note how the dark, gravel-covered regions of the natural-color image show up as the brightest (and hottest) areas in the infrared imagery of the land surface in the lower image. Lightly vegetated areas (in green, at the right edge of the image) are darker and cooler in infrared because shade and transpiration—the release of moisture by plants—cool the surface slightly. Likewise, the brightest sands in the top image are comparatively cooler in infrared because they reflect more sunlight.
