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Underwater Bear, 1999 (mixed media on paper)
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World Breaking Glass
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Climate Changes
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Yellow Climate (Homage to the Square) 1962 (oil on board)
Arc of the Diver, 2016, (oil on canvas)
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The Earth 650 million years ago - Artist's view - Snowball Earth - The Earth seen in a period of glaciation (Varanger glaciation), about 650 to 630 million years ago. This is how the Earth may have appeared about 650 million years ago during a period when snow and ice may have covered most, if not all, of the Earth's surface and oceans. This image suggests the Earth's appearance during the Marinoan glaciation from 650 to 630 million years ago. The southern and eastern hemispheres are dominated by glacier - covered land masses while the opposing hemisphere is frozen ocean save for a few areas of exposed liquid water, AKA refugia for the Earth's surviving soft - bodied multicellular organisms. In addition to the Marinoan glaciation there may have been at least two, and possibly three previous Proterozoic glacial periods going back to two billion years ago. The causes of these snowball periods are unknown but may have been due to massive volcanic eruptions, massive meteoritic impacts (both resulting in global sun - reflecting ash clouds), or variance's in the Earth's orbit
Ice Edge, 2016, (oil on canvas)
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LI Flags, 90◦S, Cortada
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The Earth 600 million years ago - Artist's view - Ediacaran Earth - The Earth seen about 600 million years ago after an important period of glaciation. This is how the Earth may have appeared 600 million years ago following the Cryogenian “” Snowball Earth”” period. The worldwide glaciers have melted and the ocean is largely liquid again. During this, the Ediacaran period, it is hypothesized that all of the Earth's landmasses had merged into a single supercontinent known as Pannotia, also known as the Vendian supercontinent. Surrounding this massive landmass is the vast Panthalassic Ocean, also known as Panthalassa. While the ocean was home to a variety of evolving multicellular life forms including the ubiquitous Dickinsonia costata, it is not believed that life had moved to dry land with possible exception of bacteria and other microbial colonies
Ursus Maritimus, 1999 (charcoal & conte on paper)
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Deep Blue, 2016 (oil on canvas)
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Love in a Cold Climate
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Ice Bear, 1998 (mixed media on paper)
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Arctic ice has its minimum, September 2018 (photo)
Ice Loss in Glacier National Park, 2006
Ice Loss in Glacier National Park, 2009
Ice Loss in Glacier National Park, 2015
Ice Loss in Glacier National Park, 2003
Woman wearing a bag with the slogan “Let's change the system, not the climate” (photo)
Laminate structures near the north pole on Mars - Layers Exposed at North Polar Cap on Mars: Laminated structures near the north polar cap of Mars. These different layers of ice and girders correspond to climatic variations over the last ten thousand years. Image obtained on 18 April 2016 by the HIRISE camera on board the Mars Reconnaissance orbiter probe. HIRISE is a 50 cm telescope that observes visible and near infrared. At the edge of Mars' permanent North Polar cap, we see an exposure of the internal layers, each with a different mix of water ice, dust and dirt. These layers are believed to correspond to different climate conditions over the past tens of thousands of years. When we zoom in closer, we see that the distinct layers erode differently. Some are stronger and more resistant to erosion, others only weakly cemented. The strong layers form ledges
Ice Loss in Glacier National Park, 1993
Ice Loss in Glacier National Park, 1998
The coldest place on Mars - Coolest place on Mars: Detail of the ice cap of the southern pole of Mars, composed mainly of carbon dioxide. This dry ice accumulates on the surface mainly in winter, the temperature of this area can sometimes drop to 130 degrees Celsius below zero. Image obtained on August 29, 2016 by the HIRISE camera on board the Mars Reconnaissance orbiter probe. HIRISE is a 50 cm telescope that observes visible and near infrared. The polar cap is made from carbon dioxide (dry ice), which does not occur naturally on the Earth. The circular pits are holes in this dry ice layer that expand by a few meters each Martian year. New dry ice is constantly being added to this landscape by freezing directly out of the carbon dioxide atmosphere or falling as snow. Freezing out the atmosphere like this limits how cold the surface can get to the frost point at -130 degrees Celsius (-200 F). Nowhere on Mars can ever get any colder this, making this coolest landscape on Earth and Mars combined
Martian dunes at the end of winter - March: Late Winter view of Dunes: Detail on dunes in the southern hemisphere of Mars. With the end of winter, the Sun melts the carbon dioxide ice present all winter. Image obtained by the HIRISE camera of the Mars Reconnaissance probe orbiter on March 21, 2016. HIRISE is a 50 cm telescope that observes visible and near infrared. Sand dunes cover much of this terrain, which has large boulders lying on flat areas between the dunes. It is now late winter here in the Southern hemisphere, and these dunes are just getting enough sunlight to start defrosting their seasonal cover of carbon dioxide. Spots form where pressurized carbon dioxide gas escapes to the surface
Anacortes Smokeshow, c. 2024 (charcoal, watercolor and casein on paper)
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Martian dunes in winter - March: Winter view of Dunes - Detail on dunes in a crater located in the southern hemisphere of Mars. Clearly, areas covered with gel appear on this image obtained by the HIRISE camera of the Mars Reconnaissance probe orbiter on November 25, 2006. HIRISE is a 50 cm telescope that observes visible and near infrared. Dunes within a crater on Mars are visible in this HiRise image. This crater is located in the southern hemisphere where it was winter at the time this image was taken on November 25, 2006. This observation documents new seasonal processes occurring on dunes at this latitude, as well as other interesting phenomena. The bright tones are interpreted as carbon dioxide or water frost. This is generally concentrated on the east - facing slopes of the dunes, which are in shadow and therefore cooler. Some dark spots on the dunes may be areas that have defrosted more than surrounding terrain. Landslides and dark - toned streaks are seen on many of the west - facing dune slopes. The general dune morphology indicates formation by westerly winds
Mars: Sedimentary layers in Becquerel crater - Mars: Periodic Layering in Becquerel Crater - Detail on sedimentary layers in Becquerel crater (Arabia Terra region), obtained on June 10, 2007 by the HIRISE camera on board the Mars Reconnaissance orbiter probe. This image in false colors shows sedimentary rocks in pink, sand in blue. The study of these sedimentary depot strata suggests that the climate of Mars is linked to the inclination of the axis of rotation of the planet. Rhythmic bedding in sedimentary bedrock within Becquerel crater on Mars is suggested by the patterns in this image from the High Resolution Imaging Science Experiment (HiRise) camera on Nasa's Mars Reconnaissance Orbiter. Three dimensional analysis based on stereo pairs of images confirmed the regularity of repetition in the thickness of the beds. In the top half of this image, some of the rhythm is apparent as a series of bundles of about 10 individual layers per bundle. By corresponding to a known 10 - to - one pattern in changes in the tilt of Mars' rotation axis, this pattern suggests the periodicity in the rock layers results from cyclical changes in the planet's tilt. Individual layers in the scence average 3.6 meters (12 feet) thick. The view is presented in enhanced color emphasizing the differing compositions of surface material. Sand trapped in relative low points in the terrain appears blue. Sedimentary rocks appear pink. This image was taken on June 10, 2007. The location of the imaged area is at 22 degrees north latitude, 352 degrees east longitude, within the Arabia Terra region
Hurricane Dorian - August 2019
Glaciation on Earth and Early Moon - Artist's View - Snowball Earth and Early Moon - The Earth seen in a period of glaciation several billion years ago.
The Earth seen in a period of glaciation several billion years ago.
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Polar Bear (mixed media on paper)
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Snow on Mars - Illustration - Snow at the martian pole: Snow Tempete at the martian pole
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Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
A paper and bamboo sunshade
Martian dunes in Spring - March: Frost - covered dunes in crater - Detail on dunes in a crater located near the north pole of Mars. Clearly, areas covered with carbon dioxide gel appear on this image obtained by the HIRISE camera of the Mars Reconnaissance probe orbiter on January 1, 2010. HIRISE is a 50 cm telescope that observes visible and near infrared Dunes are often found on crater floors. In the winter time at high northern latitudes the terrain is covered by carbon dioxide ice (dry ice). In the spring as this seasonal ice evaporates many unusual features unique to Mars are visible. On the floor of this crater where there are no dunes, the ice forms an uninterrupted layer. On the dunes however, dark streaks form as surface material from below the ice is mobilized and deposited on top of the ice. In some cases this mobile material probably slides down the steep face of the dune, while in other cases it may be literally blown out in a process of gas release similar to removing a cork from a champagne bottle. Image taken on 1 January 2010 by Mars Reconnaissance Orbiter (MRO) spacecraft
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Lignite-fired power plant, Germany 1979
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Floods, 2015 (ink on the paper and watercolour)
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Pratab Nagar, CLIMATE CHANGE 2021 (photograph)
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Colorado Rocky Mountains snow
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Mother and Twins, 2015 (w/c and gouache on paper)
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Thawing of glaciers with lateral and terminal moraines
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Fog banks in the valleys of Lomagne (32) - Hazy morning - Fog banks in the valleys of Lomagne, Gers. Haze in Lomagne area, Gers, France
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
Misty morning in gascogne - Hazy morning - Fog banks in the valleys of Lomagne, Gers. Haze in Lomagne area, Gers, France
Moon Bears, 2016 (oil on canvas)
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Martian dunes in Spring - March: Spring view of Dunes - Detail on sand dunes near the north pole of Mars. These dunes are covered with carbon dioxide gel during the Martian winter. In spring, dark streaks appear, sand flows caused by the degel. Image obtained by the HIRISE camera of the Mars Reconnaissance probe orbiter on April 7, 2008. HIRISE is a 50 cm telescope that observes visible and near infrared. Falling Material Kicks Up Cloud of Dust on Dunes. There is a vast region of sand dunes at high northern latitudes on Mars. In the winter, a layer of carbon dioxide ice covers the dunes, and in the spring as the sun warms the ice it evaporates. This is a very active process, and sand dislodged from the crests of the dunes cascades down, forming dark streaks. In thid image falling material has kicked up a small cloud of dust. The color of the ice surrounding adjacent streaks of material suggests that dust has settled on the ice at the bottom after similar events. Also discernible in this subimage are polygonal cracks in the ice on the dunes (the cracks disappear when the ice is gone). Image taken on 07 April 2008 by Mars Reconnaissance Orbiter (MRO) spacecraft
Earth 443 million years ago - Artist View - Silurian Earth - This is how the Earth may have appeared 443 million years ago during the Silurian period. The northern most continent is what would become today's Siberia and to the west of that is the Panthalassic Ocean. South of the equator to the east is the early - Palaeozoic continent of Baltica later to form part of Eurasia, while to the east is the continent of Laurentia later to become the core of North America. Further south is the Rheic Ocean and to the west the Iapetus Ocean
Northern Lights, 1998 (mixed media on paper)
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Arctic, 1999 (charcoal & conte on paper)
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Cirrus clouds - floccus species against a pale blue sky
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Beach Climate Tides, 2023 (photo)
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November 2007 Temperature Map - Land surface temperatures in november 2007 - Map of average temperatures observed on Earth's surface by the Terra satellite between November 1 and December 1, 2007. The coldest regions appear in blue and white, the warmest in yellow and red. Moderate Resolution Imaging Spectroradiometer (MODIS) flying on NASA's Terra satellite between November 1 and December 1, 2007. It shows how the indirectness of sunlight at high latitudes affects temperature. The coldest areas, colored blue and white, are in the north, while the warmest areas, yellow and red, are near the Equator. These are also the planet's most snow - covered areas
Forest dieback as a topic at the Rose Sunday procession, 1981
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Accustomising oneself to the vagaries of our climate..
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Earth: biosphere map - Global Biosphere - Map of mean concentration of chlorophyll and vegetation between 1997 and 2000. It is with great pleasure that the Sea - viewing Wide Field - of - view Sensor (SeaWIFS) Project announces that September 18, 2000, was the third anniversary of the start of SeaWIFS observations of this remarkable planet called Earth. This SeaWIFS image of our world depicts the global biosphere - - the ocean's long - term average phytoplankton chlorophyll concentration acquired between September 1997 and August 2000 combined with the SeaWIFS - derived Normalized Difference Vegetation Index over land during July 2000. This image shows where there is more or less plant life on our planet. On land, the dark greens show where there is abundant vegetation and tans show relatively sparse plant cover. In the oceans, red, yellow, and green pixels show dense phytoplankton blooms while blues and purples show where there is very little of the microscopic marine plant
Tempete Xynthia above France seen by satellite - Storm Xynthia above France seen by satellite - The Xynthia tempete seen by Aqua satellite on 27 February 2010. An extratropical cyclone named Xynthia brought hurricane - force winds and high waves to Western Europe. Winds as fast as 200 kilometers (125 miles) per hour reached as far inland as Paris, and at the storm's peak, hurricane - force winds extended from Portugal to the Netherlands. Hundreds of people had to take refuge from rising waters on their rooftops. By March 1, at least 58 people had died, some of them struck by falling trees. Most of the deaths occurred in France, but the storm also caused casualties in England, Germany, Belgium, Spain, and Portugal. The Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA's Aqua satellite captured this image of Western Europe, acquired in two separate overpasses on February 27, 2010. MODIS captured the eastern half of the image around 10:50 UTC, and the western half about 12:30 UTC. Forming a giant comma shape, clouds stretch from the Atlantic Ocean to northern Italy
barometer is a scientific instrument used in meteorology
Landscape and fauna of equatorial forest, Drawing
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