acquired February 24 - April 25, 2018
acquired April 25, 2018
A Pulse of Green in Australia
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Metadata
- Sensor(s):
- Landsat 8 - OLI
- Data Date: February 24, 2018 - April 25, 2018
- Visualization Date: May 3, 2018
The Lake Eyre Basin in the interior of Australia is among the driest places on the continent. With less than 125 millimeters (5 inches) of rain falling in this area each year, the streams and creeks that drain into Lake Eyre—the lowest point in Australia—are usually bone dry, barren, and brown.
Occasionally, the channels do fill after heavy downpours—and create a carpet of green. The Operational Land Imager (OLI) on Landsat 8 observed this transformation in a series of false-color images (bands 6-5-3) acquired between February 24 and April 25, 2018. With this band combination, flood water appears light blue. Vegetation is light green.
The Diamantina River flows southwest from northern Queensland toward Lake Eyre in South Australia. In February 2018, its channels were brown and parched. But after a series of storms in March 2018 dumped heavy rain in northern Queensland, water spread across its broad, braided river channels. By April, an expanse of green had emerged in the floodplain after the water receded.
“Ephemeral sedges, reeds, and grasses germinate while the floodplain is inundated,” explained Kenneth Clarke, a University of Adelaide scientist. “The whole life cycle of these species has evolved to take advantage of occasional, short pulses of floodwaters. As the waters recede, the plants finish growing, flower, and set seed—all before the moisture in the soil has been exhausted.”
It is relatively common for the Diamantina River channel and other waterways that connect to Lake Eyre to go green. For instance, a major flood and greening event affected the basin in 2011.
Typically, Lake Eyre fills up about once per decade, though the Diamantina River does deliver small amounts of water roughly every other year. Water from the current pulse of flooding has not yet advanced all the way to Lake Eyre, and there may not be enough water to make it there. Typically, most of the flood water is lost to evaporation and transpiration.
Satellites offer a powerful tool for tracking flooding and greening events, explained Clarke, the co-author of a Goyder Institute report that detailed how vegetation in the basin responds to inundation. “Too often these events are studied at only a few locations and at a few points in time,” he said. “These events can affect huge areas for a long time, but the specific timing, frequency, and duration has not been well studied.”
In addition to providing opportunities for science, greening events offer locals a chance for recreation as well. “Some people make special trips to drive through the region or camp for a while, just to experience the flush of vegetation in the desert and all the wildlife—birds and insects, and some larger animals—that follow,” said Clarke.
Further Reading
- ABC News (2018, April 9) After a rainfall, where does all the water go? Accessed May 2, 2018.
- Australian Government Lake Eyre Basin. Accessed May 2, 2018.
- Bureau of Meteorology (2018, March) Lake Eyre Basin - March 2018 Summary. Accessed May 2, 2018.
- Bureau of Meteorology (2010) Lake Eyre Basin. Accessed May 2, 2018.
- Goyder Institute (2015) Spatial Indicators of Ecological Condition for Lake Eyre Basin. Accessed May 2, 2018.
NASA Earth Observatory images by Joshua Stevens, using Landsat data from the U.S. Geological Survey. Story by Adam Voiland.
This image record originally appeared on the Earth Observatory. Click here to view the full, original record.