Skip to main content

#Landsat #NASA #USGS #Earth. Great Bahama Bank


When oceanographer Serge Andréfouet first saw a satellite image of the Great Bahama Bank, he knew the colors and contours were special. He passed the unique image to a colleague, who submitted it to NASA's Earth Observatory (EO) for an Image of the Day in 2002 (top image). Nearly eighteen years later, the image is still much appreciated. In fact, it knocked off more recent satellite imagery to win EO's Tournament Earth 2020.

"There are many nice seagrass and sand patterns worldwide, but none like this anywhere on Earth," said Andréfouet, who is now studying reefs at the Institute for Marine Research & Observation in Indonesia. "I am not surprised it is still a favorite, especially for people who see it for the first time." He said the image has been featured over the years on numerous websites, in books, and even at rave parties.

The varying colors and curves remind us of graceful strokes on a painting, but the features were sculpted by geologic processes and ocean creatures. The Great Bahama Bank was dry land during past ice ages, but it slowly submerged as sea levels rose. Today, the bank is covered by water, though it can be as shallow as two meters (seven feet) deep in places. The bank itself is composed of white carbonate sand and limestone, mainly from the skeletal fragments of corals. The Florida peninsula was built from similar deposits.

Andréfouet's image (top) shows a small section of the bank as it appeared on January 17, 2001, and was acquired by the Enhanced Thematic Mapper Plus (ETM+) on the Landsat 7 satellite (using bands 1-2-3). At that time the instrument's blue channel (band 1) helped distinguish shallow water features better than previous satellite mission.

The wave-shaped ripples in the images are sand on the seafloor. The curves follow the slopes of underwater dunes, which were probably shaped by a fairly strong current near the sea bottom. Sand and seagrass are present in different quantities and at different depths, which gives the image a range of blues and greens. The area appeared largely the same when Landsat 8 passed over on February 15, 2020.

The shallow bank quickly drops off into a deep, dark region known as the "Tongue of the Ocean." Diving about 2,000 meters (6,500 feet) deep, the Tongue of the Ocean is home to more than 160 fish and coral species. It lies adjacent to the Andros Island, the largest in the Bahamas and one of the largest fringing reefs in the world. The image above was acquired on April 4, 2020, by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA's Terra satellite.

At the time of the 2001 image, researchers did not have a good understanding of the location and distribution of reef systems across the world. Global maps of coral reefs had not changed much since the 19th Century. So researchers turned to satellites for a better view. Andréfouet's image was collected as part of the NASA-funded Millennium Coral Reef Mapping Project, which aimed to image and map coral reefs worldwide. The project gathered more than 1,700 images with Landsat 7, the first Landsat to take images over coastal waters and the open ocean.

Today, many satellites and research programs continue to map and monitor coral reef systems, and marine scientists have a better idea of where the reefs are and how they are faring. Researchers now use reef images and maps in tandem with sea surface temperature data to identify areas vulnerable to coral bleaching.

NASA Earth Observatory images by Joshua Stevens, using Landsat data from the U.S. Geological Survey, and MODIS data from NASA EOSDIS/LANCE and GIBS/Worldview.2002 imagery courtesy Serge Andrefouet, University of South Florida. Story by Kasha Patel.


#Landsat #NASA #USGS #Earth


....

Vineesh V
Assistant Professor of Geography,
Directorate of Education,
Government of Kerala.
https://g.page/vineeshvc

Comments

Popular posts from this blog

Geography of Landslides. Mitigation and Resilience.

A landslide is a geological event in which a mass of rock, earth, or debris moves down a slope under the force of gravity. Landslides can range in size from small to large and can be triggered by natural events such as heavy rainfall, earthquakes, or volcanic activity, or by human activities such as construction or mining. The geography of landslides is affected by a variety of factors that can increase the likelihood of landslides occurring in a particular area. These factors include slope angle and steepness, the type of soil and rock present, the climate and weather patterns of the region, the presence or absence of vegetation, and human activities such as construction, mining, and deforestation. Areas with steep slopes are more prone to landslides because gravity has a stronger effect on loose soil and rock, making it more likely to move downhill. Similarly, areas with loose, sandy soil or weak, fractured rock are more prone to landslides because they are less stable and more easil...

Geography of Flood. Types. Charector.

The geography of floods refers to the characteristics and patterns of floods in different geographic regions. Floods can occur in various landscapes, such as mountains, plains, coastal areas, and urban environments. The geography of a region plays a significant role in determining the frequency, magnitude, and impacts of floods. Some of the factors that influence the geography of floods include: Topography: The shape and elevation of the land can affect the flow and accumulation of water during a flood. For example, flat terrain can lead to slow-moving and widespread flooding, while steep slopes can result in flash floods and landslides. Climate: Regions with high rainfall or snowmelt can experience more frequent and intense floods, while dry regions may experience flash floods due to sudden, heavy rainfall. Hydrology: The characteristics of a river basin, such as its size, shape, and water flow, can influence the severity of a flood. For example, large river basins with extensive floo...

Landslides. USGS

Landslides. TYPES OF LANDSLIDES The term "landslide" describes a wide variety of processes that result in the downward and outward movement of slope-forming materials including rock, soil, artificial fill, or a combination of these. The materials may move by falling, toppling, sliding, spreading, or flowing. The animated GIF shows a graphic illustration of different types of landslides, with the commonly accepted terminology describing their features. The various types of landslides can be differentiated by the kinds of material involved and the mode of movement.

Flood prone regions India

Floods are natural disasters characterized by the overflow of water onto normally dry land. Various factors contribute to floods, including intense rainfall, rapid snowmelt, storm surges from coastal storms, and the failure of dams or levees. The geographical explanation involves understanding the key components of flood-prone regions: 1. Proximity to Water Bodies:    Flood-prone regions are often situated near rivers, lakes, or coastal areas. These locations are more susceptible to flooding as they are in close proximity to large water sources that can overflow during heavy precipitation or storms. 2. Topography:    Low-lying areas with gentle slopes are prone to flooding. Water naturally flows to lower elevations, and flat terrains allow water to accumulate easily. Valleys and floodplains are common flood-prone areas due to their topographical characteristics. 3. Rainfall Patterns:    Regions with high and concentrated rainfall are more likely to experience flooding. Intense and prol...

Volcano

Large magma chamber Bedrock Conduit (pipe) Base Sill Dike Layers of ash emitted by the volcano Flank Layers of lava emitted by the volcano Throat Parasitic cone Lava flow Vent Crater Ash cloud