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by National Aeronautics




  National Aeronautics and

  Space Administration

  The poetry of earth is ceasing never.

  —John Keats

  “On the Grasshopper and Cricket”

  Library of Congress Cataloging-in-Publication Data Names: Carlowicz, Michael J., author. | Friedl, Lawrence, author. | Ward, Kevin A., 1968- author. | United States. National Aeronautics and Space Administration, issuing body.

  Title: Earth / Michael Carlowicz, Lawrence Friedl, Kevin Ward.

  Description: Washington, DC : National Aeronautics and Space Administration, Earth Science, NASA Headquarters, [2018]

  Identifiers: LCCN 2018048628| ISBN 9781626830479 (hardback) | ISBN 1626830479

  (hardback)

  Subjects: LCSH: Earth (Planet)--Photographs from space. | Earth

  (Planet)--Remote-sensing images. | Earth (Planet)

  Classification: LCC QB637 .C37 2018 | DDC 910.020222--dc23 | SUDOC NAS 1.2:EA 7/21

  LC record available at https://lccn.loc.gov/2018048628

  THRAE

  ii

  Contents

  vi Foreword

  2 Atmosphere

  4

  Curving Cloud Streets, Brazil and Bolivia

  6

  A Trio of Plumes, South Atlantic Ocean

  8

  Filling the Valleys, Peru

  10

  A Glorious View, Pacific Ocean

  12

  Punching Holes in the Sky, United States

  14

  Bering Streets, Arctic Ocean

  16

  Riding the Waves, Mauritania

  18

  Cloud Shadow, Germany

  20

  Double Trouble, Pacific Ocean

  24

  Making Tracks, Pacific Ocean

  26

  Tracing the Coast, China

  28

  Four Mountains Stand Out, Pacific Ocean

  32

  Framing an Iceberg, South Atlantic Ocean

  sTn

  34

  Valley Fog, Canada

  eT

  36

  Holuhraun Lava Field, Iceland

  n

  38

  Lofted Over Land, Madagascar

  Co

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  iv

  40 Water

  118

  Taranaki and Egmont, New Zealand

  42

  Channel Country, Australia

  120

  Cultivating a Border, China and Kazakhstan

  44

  Tea-Colored Rupert Bay, Canada

  122

  Barrier Islands, Brazil

  48

  Coral Cocos, Indian Ocean

  124

  Tsauchab River Bed, Namibia

  50

  Bay of Whales, Russia

  126

  Ice and Snow

  52

  Storms Stir Up Sediment, Bermuda

  128

  Mertz Loses Part of Its Tongue, Antarctica

  54

  The Meeting of the Waters, Brazil

  130

  Swimming with Ice Cubes, United States

  56

  A Lava Lamp Look at the Atlantic, Atlantic Ocean

  132

  Franz Josef Land, Arctic Ocean

  58

  Teeming Life in the Strait of Georgia, Canada

  134

  No Green in This Land, Greenland

  60

  Ephemeral Lake Frome, Australia

  136

  Mackenzie Meets Beaufort, Canada

  62

  Dueling Blooms, Barents Sea

  138

  Sea Ice at Shikotan, Japan and Russia

  64

  A Bay Sculpted by Ice, Canada

  140

  North Patagonian Icefield, South America

  66

  Tidal Flats and Channels, Bahamas

  144

  Manning Island and Foxe Basin, Canada

  68

  The Blooming Baltic, Baltic Sea

  146

  Ice Water, United States

  70

  Waves Beneath the Waves, Trinidad

  148

  Omulyakhskaya and Khromskaya, Russia

  72

  Land of Lakes, Canada

  150

  Phytoplankton on Ice, Antarctica

  74

  Plankton and Sulfur, Namibia

  152

  Heart-Shaped Uummannaq, Greenland

  76

  Åland Islands, Scandinavia

  154

  Puma Yumco, China

  78

  Crater Lakes with Clear Water, Canada

  156

  Grounded in the Caspian, Kazakhstan

  80

  Mergui Archipelago, Southeast Asia

  158

  Ice-Covered Delta, Canada

  82

  Scarlet Lake Natron, Tanzania

  160 Appendix

  84

  Swirling Bloom off Patagonia, Argentina

  164 Acknowledgments

  86 Land

  88

  A Curious Ensemble of Wonderful Features, United States

  166 Credits

  92

  Megadunes and Desert Lakes, Mongolia

  168

  About the Authors

  94

  Colorful Faults of Xinjiang, China

  96

  Bowknot Bend, United States

  98

  From Rainforest to Rain Shadow, United States

  100

  A Blaze of Color, Sweden

  102

  Folds and Curves of the Kavir, Iran

  104

  Fanning Out in Farmland, Kazakhstan

  108

  The Zones of Kilimanjaro, Tanzania

  110

  Liwa Oasis, United Arab Emirates

  112

  Don Juan Pond, Antarctica

  114

  Linear Dunes, Caprivi Strip, Namibia

  116

  Harratt Lunayyir Lava Field, Saudi Arabia

  Foreword

  of all celestial bodies within reach or view, as far as we can

  see, out to the edge, the most wonderful and marvelous and

  mysterious is turning out to be our own planet earth. There is

  nothing to match it anywhere, not yet anyway.

  —Lewis Thomas

  Sixty years ago, with the launch of Explorer 1, NASA made

  its first observations of Earth from space. Fifty years ago,

  astronauts left Earth orbit for the first time and looked back

  at our “blue marble.” All of these years later, as we send

  spacecraft and point our telescopes past the outer edges of

  the solar system, as we study our planetary neighbors and

  our Sun in exquisite detail, there remains much to see and

  explore at home.

  dRo

  We are still just getting to know Earth through the tools of

  we

  science. For centuries, painters, poets, philosophers, and

  Ro

  photographers have sought to teach us something about our

  F

  home through their art.

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  vi

  This book stands at an intersection of science and art. From NASA has a unique vantage point for observing the beauty and

  its origins, NASA has studied our planet in novel ways, using

  wonder of Earth and for making sense of it. Looking back from

  ingenious tools to study physical processes at work—from

  space, astronaut Edgar Mitchell once cal ed Earth “a sparkling

  beneath the crust
to the edge of the atmosphere. We look at it

  blue and white jewel,” and it does dazzle the eye. The planet’s

  in macrocosm and microcosm, from the flow of one mountain

  palette of colors and textures and shapes—far more than just

  stream to the flow of jet streams. Most of al , we look at Earth blues and whites—are spread across the pages of this book.

  as a system, examining the cycles and processes—the water

  We chose these images because they inspire. They tell a story

  cycle, the carbon cycle, ocean circulation, the movement of

  of a 4.5-bil ion-year-old planet where there is always something heat—that interact and influence each other in a complex,

  new to see. They tell a story of land, wind, water, ice, and air dynamic dance across seasons and decades.

  as they can only be viewed from above. They show us that no

  We measure particles, gases, energy, and fluids moving in, on,

  matter what the human mind can imagine, no matter what the

  and around Earth. And like artists, we study the light—how it

  artist can conceive, there are few things more fantastic and

  bounces, reflects, refracts, and gets absorbed and changed.

  inspiring than the world as it already is. The truth of our planet Understanding the light and the pictures it composes is no

  is just as compel ing as any fiction.

  small feat, given the rivers of air and gas moving between our

  We hope you enjoy this satel ite view of Earth.

  satel ite eyes and the planet below.

  It is your planet. It is NASA’s mission.

  For all of the dynamism and detail we can observe from orbit,

  Michael Carlowicz

  sometimes it is worth stepping back and simply admiring Earth.

  It is a beautiful, awe-inspiring place, and it is the only world most of us will ever know.

  The astonishing thing about the Earth…

  is that it is alive.... Aloft, floating free

  beneath the moist, gleaming membrane

  of bright blue sky, is the rising Earth, the

  only exuberant thing in this part of the

  cosmos…. It has the organized,

  self-contained look of a live creature,

  full of information, marvelously skilled

  in handling the Sun.

  —Lewis Thomas

  The Lives of a Cel

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  2

  atmosphere

  Curving Cloud Streets

  Brazil and Bolivia

  To the human eye, the wind is invisible. It can only be visualized by proxy, by its expressions in other phenomena like blowing leaves, airborne dust, white-capped waters—or the patterns of clouds.

  Acquired in June 2014 by the Aqua satel ite, this image shows a broad swath of the Amazon rainforest in Brazil and Bolivia as it appeared in the early afternoon. As sunlight warms the forest in the morning, water vapor rises on columns of heated air. When that humid air runs into a cooler, more stable air mass above, it condenses into fluffy cumulus clouds.

  Cumulus cloud streets often trace the direction, and sometimes the intensity, of winds—lining up paral el to the direction of the wind.

  Usual y this means a straight line, but clouds can also line up along the concentric, curved lines of high-pressure weather systems, as they did here.

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  A Trio of Plumes

  South Atlantic Ocean

  The uninhabited South Sandwich Islands include several active stratovolcanoes. Due to their remote location, these volcanoes are some of the least studied in the world, though satel ites often catch them erupting.

  The combination of clouds and ice at these latitudes can make it difficult to see plumes of volcanic ash in natural-color imagery.

  But using portions of the electromagnetic spectrum that are typical y invisible to the naked eye (such as infrared) enables satel ites to distinguish ice from ash and clouds. The Aqua satel ite captured this false-color image in September 2016. Note the three bright white plumes running down the middle third of the page; they are warmer and brighter in infrared than the cooler ice clouds (teal) around them.

  Researchers have learned that even small eruptions like this can affect cloud cover and weather. The tiny solid and liquid particles in the plume (aerosols) act as seeds for the formation of cloud droplets.

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  Filling the Valleys

  Peru

  The val eys along Peru’s southern coast are among the deepest on Earth. They are also frequently fil ed with clouds. In July 2015, Landsat 8 captured this view of the cloud-fil ed canyons through which the Yauca and Acarí rivers empty into the Pacific Ocean.

  You can’t see it, but the Pacific lies below the clouds on the lower left. The clouds are marine stratocumulus—a type of low-level cloud so close to the surface that it is essential y fog. Such clouds are a persistent feature off the coast of Peru and Chile, developing most often during the winter and early spring. On some occasions, prevailing winds can push the clouds inland.

  Because the marine clouds are low, they are easily blocked by coastal mountains and hil s, such as the Andes. But in areas where low val eys open to the ocean, the clouds move inland.

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  A Glorious View

  Pacific Ocean

  A layer of stratocumulus clouds over the Pacific Ocean serves as the backdrop for this rainbow-like phenomenon known as a glory.

  Glories form when water droplets within clouds scatter sunlight back toward a source of il umination (in this case, the Sun).

  Although glories may look similar to rainbows, the way light is scattered to produce them is different. Rainbows are formed by refraction and reflection; glories are formed by backward diffraction. From the ground or from an airplane, glories appear as circular rings of color. In this image, however, the glory is stretched vertical y because of how the imager scans the surface in swaths.

  Note, too, the swirling von Kármán vortices visible to the right of the glory. The alternating rows of vortices form as air masses run into an obstacle—the island of Guadalupe—and form a wake behind it.

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  Punching Holes in the Sky

  United States

  In December 2009, the Landsat 5 satel ite observed this extraordinary example of “hole-punch clouds” over West Virginia.

  This strange phenomenon results from a combination of cold temperatures, air traffic, and atmospheric instability.

  If you were to look from below, it would appear as if part of the cloud were fal ing out of the sky. As it turns out, that is actual y what is happening. The clouds are initial y composed of liquid drops at a super-cooled temperature below 0° Celsius. As an airplane passes through a cloud, particles in the exhaust can create a disturbance that triggers freezing. Ice particles then quickly grow at the expense of water droplets. Eventual y, the ice crystals in these patches of clouds grow large enough that they literal y fall out of the sky, earning hole-punch clouds their alternate name: “fal streak holes.”

  In this false-color image, pink and faint blue areas are typical water-rich clouds, and bright cyan areas are ice clouds.

  The hole-punch areas appear dark around the ice clouds.

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  Bering Streets

  Arctic Ocean

  Winds from the northeast pushed sea ice southward and formed cloud streets—paral el rows of clouds—over the Bering Strait in January 2010. The easternmost reaches of Russia, blanketed in snow and ice, appear in the upper left. To
the east, sea ice spans the Bering Strait. Along the southern edge of the ice, wavy tendrils of newly formed, thin sea ice predominate.

  The cloud streets run in the direction of the northerly wind that helps form them. When wind blows out from a cold surface like sea ice over the warmer, moister air near the open ocean, cylinders of spinning air may develop. Clouds form along the upward cycle in the cylinders, where air is rising, and skies remain clear along the downward cycle, where air is fal ing. The cloud streets run toward the southwest in this image from the Terra satel ite.

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  Riding the Waves

  Mauritania

  You cannot see it directly, but air masses from Africa and the Atlantic Ocean are col iding in this Landsat 8 image from August 2016.

  The col ision off the coast of Mauritania produces a wave structure in the atmosphere.

  Cal ed an undular bore or solitary wave, this cloud formation was created by the interaction between cool, dry air coming off the continent and running into warm, moist air over the ocean. The winds blowing out from the land push a wave of air ahead like a bow wave moving ahead of a boat.

  Parts of these waves are favorable for cloud formation, while other parts are not. The dust blowing out from Africa appears to be riding these waves. Dust has been known to affect cloud growth, but it probably has little to do with the cloud pattern observed here.

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  Cloud Shadow

  Germany

  In November 2012, the Earth Observing-1 satel ite acquired this image of a layer of clouds casting a distinctive shadow on another, lower cloud layer. The upper deck was more than 1 kilometer (0.6 miles) above the ground. Both layers were composed of stratus clouds, a low-lying type that tends to be uniform and flat. When the satel ite’s Advanced Land Imager acquired the image, the clouds were over northeastern Germany near Harz National Park.

  While local meteorological conditions affect cloud height, the latitude at which clouds form is also important. Almost all clouds exist in the lowest level of the atmosphere, the troposphere. However, the depth of the troposphere varies by latitude—thinner near the poles than the Equator, so clouds can occur at higher levels in the tropics than they do at high- and mid-latitudes.

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  Double Trouble

  Pacific Ocean

 

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