February 2nd, 2021 by Brian Campbell, NASA Wallops and GLOBE
Trees connect us scientifically, environmentally, and culturally. We all know that trees are vital to our planet’s health. As trees grow, they absorb carbon from the atmosphere, playing a vital role in Earth’s global carbon cycle and helping to regulate Earth’s carbon budget.
But before you read any further, look around…especially if you are outside. Most of you can look in any direction and see a tree. You might wonder about a few things like: “What type of tree is that?” or “Why is that tree so tall or short?” or “How old is that tree?” or even “Was that tree planted by someone, or did the wind blow a seed to where the tree is now standing?”
Or what if you don’t see any trees? What does that signify about the environment? Did nature make it that way, or did humans? All of these are great questions that can help us understand and connect with the environment.
A few trees on Earth also connect us to the Moon. Have you ever heard of “Moon Trees?”
“Moon Trees” never actually grew on the Moon, but their seeds were taken into lunar orbit 50 years ago this week. The NASA Moon Trees history website explains:
Apollo 14 launched in the late afternoon of January 31, 1971, on what was to be our third trip to the lunar surface. Five days later, Alan Shepard and Edgar Mitchell walked on the Moon while Stuart Roosa, a former U.S. Forest Service smoke jumper, orbited above in the command module. Packed in small containers in Roosa’s personal kit were hundreds of tree seeds, part of a joint NASA/USFS project. Upon return to Earth, the seeds were germinated by the Forest Service. Known as the “Moon Trees,” the resulting seedlings were planted throughout the United States (often as part of the nation’s bicentennial in 1976) and the world. They stand as a tribute to astronaut Roosa and the Apollo program.
Among the Moon Trees that were eventually planted around the United States and the world were sycamores, Loblolly pines, redwoods, sweetgums, and Douglas firs. Though it is unlikely the Moon Tree seeds were changed much by their brief lunar orbit, it is still a wonder that they made it into space and back, and that many of the trees are growing and thriving today.
Perhaps you might see some Moon Trees in person in the next year or two. If you do, consider making tree height observations using the tree tools on the NASA GLOBE Observer app. When completing your observation, let us know in the app.
Have you ever visited and seen a Moon Tree? Tell us about it below.
January 27th, 2021 by Kathryn Hansen/NASA Earth Observatory, and Robie Macdonald/University of Manitoba/Dept. of Fisheries and Oceans
In a typical year, perhaps a dozen people visit Auluvik National Park in Canada’s Northwest Territories. Luckily, one of those visitors brought back some outstanding photos.
In November 2020, we highlighted a few compelling features around the Thomsen River estuary on Banks Island, including lines of sea ice tracing the shoreline and the braided pattern of the river. But there’s so much more to explore across this remote lowland tundra and river valley.
Robie Macdonald, a scientist at the University of Manitoba, shared some photos that he shot while doing fieldwork in the region between 2014 and 2016. The purpose of that project, led by Matt Alkire of the University of Washington, was to collect geochemical measurements from small rivers across the Canadian Arctic Archipelago.
“I really do love working in these places,” Macdonald said. “Once the aircraft has landed, one is bathed in a tremendous silence broken only by waves breaking on shingle. Then you have this incredible tundra spreading out toward the hills that define the river floodplain.”
Here are ten of Macdonald’s favorite photographs.
1. Ponds and Oxbows
“Numerous ponds of all sizes populate the drainage basins of Banks Island, and you can see several clusters of them in the satellite image (top), especially along the small river to the west of the Thomsen. This photograph provides a closer look at one such pond cluster. In the image, you can also see textbook oxbows, which have become the setting for more ponds.”
2. Permafrost Polygons
“During breeding season, it seems like almost every pond on Banks Island has its own population of snow geese (visible in this photo). You can also see old permafrost polygons that are now submerged within the pond. Polygons are widespread features of the permafrost in soil-rich locations and are produced over time by freeze-thaw cycles of the surface active layer. Permafrost thaw is widely impacting these regions, leading to feedbacks in the carbon system (CO2, CH4).”
3. Vibrant Vegetation
“Perhaps the most surprising characteristic of the valley bottoms in this ‘Arctic desert’ is the vibrant color of the vegetation: yellows, greens, and reds mark a dense ground cover that can be seen on the satellite image as areas with a yellowish-brownish cast.”
4. Sediment Ripples
“As a result of the strong sediment supply, the large embayment at the Thomsen River mouth has been practically filled with sediment. The shallow water reveals itself in the satellite image by the lighter-greenish tone compared to water out in the channel north of Banks Island. More evidence of the ample sediment supply can be seen in beautiful displays of sand/silt ripples in the lower river between the islands. In the satellite image (top), the ripples are almost visible as grey zones between the islands before the river enters the open bay.”
5. Ice Shoves
“When walking on these islands near the river mouth, you can see evidence of bank erosion and ‘ice shoves.’ These are produced when wind forces newly formed ice to ride up over the river bank and gouge out the top layer of the silty material that makes up these islands. Unfortunately, ice shoves are too small to show on the satellite image.”
6. Vulnerable Permafrost
“Global warming and the extensive loss of sea-ice cover in late summer have helped accelerate coastal erosion and permafrost slumping. This image shows a section of coastline just to the east of the Thomsen River mouth that consists of a lot of frozen ice. This sort of permafrost is especially vulnerable to the changing temperature regime.”
7. Erosion and Slumping
“Thaw slumps are also a sign of the permafrost warming. These can be seen just barely in the satellite image as small dark regions along cliff faces–both facing the ocean and within the river drainage basins. Erosion and slumping expose ancient organic carbon to the air and the hydrosphere, thus providing an extensive positive feedback to climate warming.”
8. Bergy Bits
“Lines of bergy bits has collected along a thin shore margin at the point where the sea bottom rapidly deepens below ice keel depths, likely at approximately 2-4 meters. Although the grounded ice bits are continually melting, they are resupplied by more ice chunks shed from the permanent pack out in the channel. Two turbid plumes supplied by a river to the west of the Thomsen easily pass through the necklace of ice.”
9. Sampling Amid an Icy Barrier
“When we were sampling the water in this region, we found this ice barrier to be a bit more of a problem to navigate in our small inflatable boats, but ice along the shore did make it simple to sample sea ice. This image shows Greg Lehn preparing to launch our boat.”
10. A Suitable Landing Spot
Sampling in the Thomson River itself was somewhat simpler, once we had found a suitable place to land the plane. This image shows Greg Lehn scoping out the shore of the Thomsen River near its mouth.”
Though gentle “effusive” eruptions have been the norm at Kīlauea across the past two centuries, the geologic record shows plenty of evidence that the volcano has had periods when violent, explosive eruptions were common. The presence of water in magma is a key factor contributing to explosive eruptions, so USGS scientists have been carefully monitoring the volcano for signs that it may be entering a more explosive and dangerous phase.
Meanwhile, satellites provide the big-picture view. Landsat satellites periodically collect multi-spectral imagery of the lake; the images at the top of this page provide a natural-color perspective. Other satellites with Interferometric Aperture Radar (InSAR) complement the ground-based GPS sites by offering a crucial, large-scale view of land deformation.
“The chance to monitor an incipient volcanic lake is not unprecedented, but it is rare,” a group of USGS geologists wrote in EOS. “Kīlauea’s crater lake provides an opportunity to improve the scientific community’s understanding of how such lakes evolve and interact with magmatic systems below.”
The striking patterns in northeastern Canada’s flood basalts tell a story of continental collisions that played out almost two billion years ago. The large-scale patterns are visible from space—a wide view that provides a sweeping perspective on the region’s steps and folds cut by faults. But look closer, and then closer again, and other patterns and details emerge.
Deanne van Rooyen, a geologist at Cape Breton University, and David Corrigan of the Geological Survey of Canada, have been doing field work in the region to better understand the details of how the flood basalts evolved. They provided the following photos as examples of some of the details that become visible when viewed close up.
As described in detail in the Image of the Day, successive layers of flood basalt eroded and formed step-like features known as “traps.” The cliff face of each flow (or series of flows) represents a step, each standing about 50 to 70 meters (160 to 230 feet) tall. The steps were later folded as ancient, stable parts of Earth’s crust collided. The steps visible in the photograph above, shot from a helicopter, show some of these step-like features amid the central part of a folded structure.
A closer look at the steps (above) reveals hexagonal columns in the flood basalts. These structures are known as “columnar jointing,” and form when layers of basalt cool and contract. They occur elsewhere around the planet too; a well-known example is the Giant’s Causeway in Northern Ireland.
This photograph shows an even closer look at the column tops. Notice the hexagonal shape of the basalt. Corrigan and Van Rooyen are working on a detailed study of these basalts, which they refer to as the “Labrador Traps.”
The video below, based on photographs taken by GLOBE citizen scientist Glenn Evans, juxtaposes satellite images and photographs taken of the sky at roughly the same place and time. The contrasting perspectives underscore how easy it can be to miss the forest for the trees — or, rather, the smoke plume for the clouds — if you aren’t careful. Kristen Weaver, the deputy coordinator for GLOBE Observer, compiled the photos and matched them with the corresponding MODIS satellite images.
Victoria and New South Wales are in the midst of one of the most severe fire seasons either state has seen in decades. After months of unusually hot, dry weather, hundreds of fires have charred an area larger than West Virginia, destroying thousands of homes and resulting in dozens of deaths.
In a recent article, we described a study of how road networks in the Congo Basin have changed over the past 15 years and how they have affected deforestation rates. Those networks have grown significantly, but not all roads lead to long-term forest destruction. By closing roads when they are no longer needed, people can help avoid permanent damage to the forest.
Though the researchers conducted much of their research via
remote sensing and computer work, they also made several trips into the Congo
Basin. Their photos shed more light on some of the economic activities in the
The Congo Basin is covered by tropical rainforests and
swamps and is famous for its rich biodiversity. At two million square
kilometers (1.2 million square miles), the Congo rainforest is the second
largest in the world and about the size of Mexico. The image above shows a
forested area near a stream in the Republic of Congo.
As road networks have expanded, the roads are bringing
people deeper into the jungle and closer to wildlife. In general, forest roads
lead to more human activity and to unregulated or destructive events, such as
poaching, mining, or illegal logging. The image below demonstrates how roads
are encroaching on wildlife habitats.
The majority of new roads are built for selective logging activities, which is one of the main economic activities in the rainforest. Companies practice selective logging where only the most valuable tree species are cut, which usually results in cutting one tree per hectare on average. In order to harvest this timber though, the companies must build roads, usually unpaved, that allow the trucks and tractors to drive deep into the forest. The photos below show scenes of timber extraction and a timber yard.
Sometimes roads are used by farmers to reach further into the forest and establish small-scale agricultural plots. The image below shows a small landholder in a forest near Mbandaka in the Democratic Republic of Congo. The woman is carrying a basket of manioc (cassava). She is also holding a maranthaceae leaf, which is commonly used for wrapping and cooking on a fire.
In the recent study, the researchers found that deforestation rates were highest around older, open roads. Specifically, the highest rates were found in the Democratic Republic of Congo due to agriculture and a high population density.
Researchers showed deforestation rates were the lowest around abandoned or closed roads. Abandoned roads reduce human traffic and allow vegetation to grow over the dirt path. The image below shows an abandoned road in the Republic of Congo that is overgrown with regenerating trees and plants. These plant species pictured are popular for gorillas to feed on and can help restore the gorillas’ natural habitat.
Abandoned roads were most commonly found inside logging concession areas. After a logging company was no longer using the road, the road was often closed or abandoned. Sometimes the road can be closed off by simply using a log to prevent vehicles from entering, as shown below.
October 4th, 2019 by Joe Atkinson, NASA Langley Research Center
Who knew that being a scientist could be as easy as pointing your phone at the sky? This month, NASA and the GLOBE Program are asking citizen scientists to take out their phones and report what kinds of clouds they see above them.
“What excites researchers about GLOBE observations is the ability to see what’s up in the sky from volunteers’ perspectives all over the world,” said Marilé Colón Robles, lead for the GLOBE Clouds Team at NASA’s Langley Research Center. “What our eyes can see is difficult to fully duplicate with instruments. Merging these views is what makes a complete and impactful story.”
“We want to do a data challenge in the fall and see if there are any differences from what was observed during the spring data challenge of 2018,” said Colón Robles. “From thin, high clouds that are hard for satellites to detect to dust storms that impact our daily lives, these observations play an important role in better understanding our atmosphere.”
At NASA, scientists work with a suite of satellite instruments known as the Clouds and the Earth’s Radiant Energy System (CERES). Though they have these highly sensitive instruments, it can sometimes be difficult for scientists to distinguish features such as cirrus clouds from snow cover in their imagery because both are cold and bright from a satellite perspective. By comparing satellite images from a particular area with data submitted by citizen scientists, researchers can differentiate between the two.
Lucky GLOBE observers might make an observation while the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) is overhead. CALIPSO is a joint mission between NASA and the French space agency (CNES) that uses laser pulses to measure clouds and atmospheric aerosols. Citizen scientists who make observations at the same time and place as CALIPSO will receive an emailed satellite comparison of CALIPSO’s measurements showing features such as high clouds, dust, and smoke. Scientists are especially interested in these observations in order to improve their understanding of dust storms. During the challenge, make sure you turn on daily satellite notifications in the app or use this satellite overpass website to see the schedule for your location.
“Last year’s challenge gave researchers special glimpses into cloud types around the world,” said Colón Robles. “Photographs provided by observers gave insight into events such as dust storms and wildfires. Our hope is to once again learn from the community and together study our atmosphere.”
The 2018 data challenge, which took place in the spring, received more than 56,000 cloud observations from more than 15,000 locations in 99 countries and Antarctica.
NASA is a sponsor of GLOBE, an international science and education program that provides students and the public with the opportunity to participate in data collection and the scientific process. NASA GLOBE Observer is a free smartphone app that lets anyone make citizen science observations from the palm of their hand.
In a recent article, we showed satellite imagery of the dramatic retreat of Alaska’s Excelsior Glacier over the past two decades. The glacier has shortened by 30 percent since 1994, primarily due to rising temperatures and calving. What was once ice is now a pool of meltwater called Big Johnstone Lake. Images collected closer to the ground also show dramatic change.
In photos taken in 1909 by the U.S. Geological Survey, Excelsior glacier nearly touched the Pacific Ocean, resting on a sliver of forested land. Today, the glacier is separated from the ocean by Big Johnstone Lake, which measures nearly five times the area of New York City’s Central Park.
The image below shows Excelsior Glacier in 2016 (first) compared to 2018 (second). While the second picture was taken from a farther distance, the absence of icebergs in Big Johnstone Lake stands out.
The following image also shows the complete separation of the glacier into its eastern and western tributaries (as seen in the top 2018 satellite photo). The owners of the lodge have named the right tributary “Roan Glacier.”
The following images show changes on Roan Glacier from 2018 to 2019. In 2019, you can see a rogue chunk of ice on right (first image below). According to the owners of the Johnstone Adventure Lodge, the chunk “was certainly not separated in September 2018,” as shown in the second picture.
This last image shows 15-20 harbor seals that hang around the glacier. Harbor seals often haul-out on icebergs, so fewer icebergs will likely mean fewer seals as time goes on.
In the early 19th century, Meriwether Lewis and William Clark led an ambitious expedition across the western United States. They greatly expanded our knowledge of the country’s geography and biological diversity through their specimen collection, mapping of the landscape, and detailed journal entries.
This year NASA and the National Park Service are encouraging the public to follow in the footsteps of Lewis and Clark through a new citizen science challenge. From June 1 to September 2, citizens are invited to use their smart phones and the NASA GLOBE Observer app to map land cover along the Lewis and Clark National Historic Trail to assist scientists studying environmental changes.
Land cover–such as grass, pavement, or trees–influences the water and energy cycles and influences a community’s vulnerability to natural disasters. NASA studies land cover changes from space as part of its mission to better understand our planet and improve lives.
To participate in the “GO on a Trail” challenge, download the free GLOBE Observer app from the Apple App Store or Google Play. Use the Land Cover tool to make observations of the landscape. Any observation made along the 5,000-mile-long Lewis & Clark trail from Pittsburgh to the mouth of the Columbia River earns points. The top participants will receive recognition and GO on a Trail commemorative material.
A good place to get started is at an observation station marked with a large sticker (image above) at Lewis and Clark visitor centers and museums. To navigate to sites of interest along the trail, the Lewis and Clark National Historic Trail and GLOBE Observer teams have provided an online map.
“We hope that by becoming involved with this project, people will care about the trail and become its stewards,” said Dan Wiley, chief of integrated resource stewardship for the Lewis and Clark National Historic Trail. Wiley notes that the challenge will both spark a general interest in science and show the public how it can be involved in collecting vital information for decision makers.
GLOBE Observer is an app-based citizen science program active in more than 120 countries. The program invites citizens to contribute land cover, cloud, mosquito, and tree height observations to NASA and the science community. NASA-funded scientists are eager to see citizen science observations of land cover along this trail because of its wide range of ecological regions. Data collected during the challenge could help improve satellite-based mapping of land cover across the continent.
“We are observing and monitoring our changing home planet from space to better understand how it is changing and what are the main drivers of change,” said Eric Brown de Colstoun, a scientist at NASA Goddard Space Flight Center. “The view from the ground provided by the challenge participants is one component that helps us verify the space-based data.”
Even if you are not able to visit the Lewis and Clark Trail this summer, you can still join the GO on a Trail challenge from any of the more than 120 countries where GLOBE Observer is active. Just get outdoors and map the land cover around you. The top participants from beyond the trail will also receive recognition and commemorative material.
“Lewis and Clark and their team were exploring a totally new environment to them,” said Brown de Colstoun. “We invite you to get out and explore, and document the places you know and care about. Go on a trail and do science along with us.”
NASA GLOBE Observer and Lewis and Clark National Historic Trail will provide regular updates about the GO on a Trail challenge via social media throughout the summer with the hashtag #GOonaTrail. Follow GLOBE Observer on Facebook @nasa.globeobserver or Twitter @NASAGO. Follow the Lewis and Clark National Historic Trail on Facebook @lewisandclarknht, Twitter @lewisclarktrail, and Instagram @lewisandclarknht or visit the website at: https://www.nps.gov/lecl/index.htm.
When we published a few Landsat images of wildflower super blooms in California in March 2019, you may have had to squint a little to find the flowers. From 705 kilometers (438 miles) above Earth’s surface, at the 15-meter-per-pixel resolution of the Operational Land Imager on Landsat 8, the flowers tend to blend with the hues of the desert.
Not so with this colorful photograph of poppies and other wildflowers in Antelope Valley that was taken from a T-34 airplane. The picture was shot by NASA Armstrong aerial photographer Jim Ross, who may have one of the coolest jobs at NASA. Watch the video below to find out how he got it.
Meanwhile, remote sensing scientist Iban Ameztoy was inspired enough by the aerial photos to pull Sentinel-2 satellite imagery of the same bloom and share them on Twitter.