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Underwater Bear, 1999 (mixed media on paper)
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World Breaking Glass
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Yellow Climate (Homage to the Square) 1962 (oil on board)
LI Flags, 90◦S, Cortada
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Climate Changes
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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
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
Deep Blue, 2016 (oil on canvas)
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Ice Edge, 2016, (oil on canvas)
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Arc of the Diver, 2016, (oil on canvas)
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Ursus Maritimus, 1999 (charcoal & conte on paper)
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Love in a Cold Climate
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Ice Loss in Glacier National Park, 2006
Ice Bear, 1998 (mixed media on paper)
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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
Arctic ice has its minimum, September 2018 (photo)
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
Ice Loss in Glacier National Park, 2009
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
Ice Loss in Glacier National Park, 2003
Ice Loss in Glacier National Park, 2015
Polar Bear (mixed media on paper)
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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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Ice Loss in Glacier National Park, 1998
Lignite-fired power plant, Germany 1979
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Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
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
Anacortes Smokeshow, c. 2024 (charcoal, watercolor and casein on paper)
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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
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
A paper and bamboo sunshade
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
Hurricane Dorian - August 2019
Mother and Twins, 2015 (w/c and gouache on paper)
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Fog banks in the valleys of Lomagne (32) - Hazy morning - Fog banks in the valleys of Lomagne, Gers. Haze in Lomagne area, Gers, France
Pratab Nagar, CLIMATE CHANGE 2021 (photograph)
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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
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
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
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
Cirrus clouds - floccus species against a pale blue sky
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Moon Bears, 2016 (oil on canvas)
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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
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
Morning mist - Hazy morning - Fog banks in the Gers (Lomagne). Haze in Lomagne area, Gers, France
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
Northern Lights, 1998 (mixed media on paper)
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Landscape and fauna of equatorial forest, Drawing
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Beach Climate Tides, 2023 (photo)
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Accustomising oneself to the vagaries of our climate..
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barometer is a scientific instrument used in meteorology
Arctic, 1999 (charcoal & conte on paper)
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100m ocean level rise - Europe - Europe with sea level+100m - Artist's view showing Europe as it would appear if the ocean level increased by 100 metres. This would happen if all glaciers on Earth melt. This is how Europe, North Africa and the Middle East may appear with mean sea level about 100 meters (330 feet) above today's. Such a dramatic rise in sea level could occur if all of the Earth's glaciers were to melt.In this image almost every European country has been flooded with sea water to some extent. Much of the United Kingdom and France have become part of the Atlantic Ocean while Denmark and The Netherlands are completely submerged as are Estonia, Latvia, and Lithuania. The Black Sea has grown to include much of Bulgaria and Ukraine.The Mediterranean Sea now covers parts of Egypt (including all of the Nile delta), Libya and Tunisia and all of western Israel. The Persian Gulf has completely submerged Kuwait, Bahrain, Qatar, and much of Iraq and United Arab Emirates. To the west some of Mauritania and all of Senegal have become part of the Atlantic Ocean
Snow Rub (Polar Bear), 2013 (watercolour and gouache on paper)
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A woman wears a gas mask during a rally of climate activists ahead of the United Nations Climate Change Conference to be held in Paris, France, from 30th November to 11th December 2015, in Frankfurt am Main, Germany, 29th November 2015 (photo)
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100m ocean level rise - South Asia - South Asia with sea level+100m - Artist's view showing South Asia as it would appear if the ocean level increased by 100 metres. This would happen if all glaciers on Earth melt. This is how South Asia may appear with mean sea level about 100 meters (330 feet) above today's. Such a dramatic rise in sea level could occur if all of the Earth's glaciers were to melt. In this image over half of Pakistan along with the Indian state of Gujarat have become part of the Arabian Sea while the Persian Gulf has consumed Iran's border with Kuwait and some of Iraq. Bangladesh has succumbed entirely to the Bay of Bengal. The Gulf of Martaban now flows into much of Myanmar
Swollen snowmelt river, Changspa, Ladakh, India (photo)