Category Archives: Eyes in the Sky

Mapping the sea surface from the Int. Space Station

The Int. Space Station is becoming a popular platform on which to experiment with and implement earth observation systems. For example, the company UrtheCast has cameras on the outside of the ISS providing continuous images of the earth. In February, a SpaceX Dragon delivered the Cloud-Aerosol Transport System (CATS) to the ISS. The CATS system will measure atmospheric aerosols and clouds. Last fall, another Dragon delivered NASA’s ISS-RapidScat instrument to the ISS where it will measures the speed of wind over the oceans.

The ISS has many advantages as a platform for testing earth observation techniques and systems.

  • Plenty of power available from its big solar panels
  • Data links, processing, and communications with earth are available.
  • The ISS’s high inclination orbit means it passes over much of the earth’s land and oceans.
  • People are available on board to install, repair, and replace the hardware.
  • New parts, replacements, etc. can be delivered and, in some cases, old parts and systems returned.

Here is a report of an ESA project to use the ISS as a platform to measure the wave heights on the oceans:

Mapping sea surface from the Space Station

16 March 2015: A new concept that involves mounting an instrument on the International Space Station and taking advantage of signals from navigation satellites could provide measurements of sea-surface height and information about features related to ocean currents, benefiting science and ocean forecasting.

ISS_for_Earth_science_node_full_image_2[1]GEROS-ISS will be installed on the upper balcony of ESA’s Columbus
space
laboratory, which provides mechanical interface plates as well
as power,
command and data links to the ISS systems.

We have all seen the beautiful photographs of our planet taken by astronauts, but orbiting Earth 16 times a day just 400 km above, the Space Station also offers a platform from which to measure certain variables related to climate change.

So, in 2011 ESA called for proposals to explore how the Space Station could be used to make scientifically valid observations of Earth. After reviewing and assessing numerous proposals, the result is to further develop the GEROS-ISS mission concept.

GEROS-ISS stands for GNSS reflectometry, radio occultation and scatterometry on board the ISS.

Global navigation satellite systems (GNSS) include GPS and Galileo satellites, which send a continual stream of microwave signals to Earth for navigation purposes, but these signals also bounce off the surface and back into space.

The idea is to install an instrument with an antenna on the Space Station that would capture signals directly from these satellites as well as signals that are reflected or scattered from Earth.

This process could be used to calculate the height of the sea surface, and to measure waves – or ‘roughness’ – that can then be used to work out the speed of surface winds.

Sea-surface_height_cm_node_full_image_2[1]Variations in sea-surface height (cm) obtained by merging multiple
altimeter measurements. GEROS-ISS would be able to observe
this variability so that maps covering latitudes 51° N to 51° S
can be produced every four days.

GEROS-ISS is primarily an experiment to demonstrate new ways of observing Earth.

However, if taken beyond the testing phase this new approach would complement measurements from satellites carrying altimeters such as CryoSat and Sentinel-3, and satellites carrying wind scatterometers such as MetOp.

Importantly, it is the first concept to assess the potential of spaceborne GNSS reflectometry to determine and map ocean height at scales of 10–100 km or longer in less than four days. Current satellite altimeters, in comparison, offer global maps at scales of around 80 km, which are produced from multiple datasets every 10 days.

A system based on GEROS-ISS would, therefore, complement existing satellite systems, helping to map ocean variability at finer spatial and temporal scales over a range of seas in tropical and temperate regions.

It would also refine our understanding of how well the concept would work for measuring the roughness of the ocean surface.

In this respect, the development of GEROS-ISS benefits from experience gained with the UK’s TechDemoSat-1, which also measures ocean-surface roughness using a similar technique. It is also hoped that NASA’s upcoming CYGNSS constellation of mini satellites will help pave the way for GEROS-ISS.

In addition, GEROS-ISS uses a technique called radio occultation whereby the antenna receives signals that are refracted as they pass through the atmosphere. This can be used to generate vertical profiles of atmospheric humidity, pressure and temperature, as does the GRAS instrument on the MetOp satellites, for example.

Jens Wickert who leads the science team that proposed GEROS-ISS said, “It is very flexible, combining different mission concepts and applications in one: GNSS-reflectometry to determine sea-surface height, scatterometry to measure sea-surface roughness and radio occultation for atmospheric studies.”

ESA engineer Manuel Martin-Neira noted, “The original concept actually goes back over 20 years and has matured considerably through numerous studies and campaigns, however, it has never been duly tested from space.”

“Being able to use the International Space Station in this way means that we can quickly validate innovative observing techniques without having to build an entire satellite, and we expect this to lead to new opportunities for science,” added Michael Kern, ESA’s GEROS-ISS mission scientist.

Jason Hatton, GEROS-ISS project coordinator, said, “The concept is still going through feasibility studies, but the aim is to launch the experiment towards the end of 2019.

Flying_over_Columbus_I_m_the_farthest_away_from_Earth_node_full_image_2[1]

This image of Europe’s Columbus space laboratory was taken by
ESA astronaut Luca Parmitano during his spacewalk on 9 July 2013.

“It would be carried to the Space Station on a cargo vehicle and installed on ESA’s Columbus space laboratory using a robotic arm, after which GEROS-ISS would run for at least a year.”

The GEROS-ISS feasibility studies are being carried out through ESA’s General Studies Programme.

Video: ESA Sentinel-2A satellite

European Space Agency’s Earth From Space webcast program reports on the Sentinel-2 earth observation satellite:

In this special edition, Wolfgang Pitz, Head of European Programmes for Airbus Defence and Space, joins the show to discuss testing the Sentinel-2A satellite at IABG in Munich, Germany. 

The Sentinel-2A is expected to be launched this summer on a Arianespace Vega rocket from Kourou, French Guiana.

Video: “Earth time lapse 2015”

Here’s a nicely made time lapse of images of earth shot from the International Space Station:

http://youtu.be/Dr_IsCQkd0s

Satellite measures the Saharan dust that keeps the Amazon fertile

The Amazon rain forest stays green because of Saharan dust:

NASA Satellite Reveals How Much Saharan Dust Feeds Amazon’s Plants

What connects Earth’s largest, hottest desert to its largest tropical rain forest?

The Sahara Desert is a near-uninterrupted brown band of sand and scrub across the northern third of Africa. The Amazon rain forest is a dense green mass of humid jungle that covers northeast South America. But after strong winds sweep across the Sahara, a tan cloud rises in the air, stretches between the continents, and ties together the desert and the jungle. It’s dust. And lots of it.

For the first time, a NASA satellite has quantified in three dimensions how much dust makes this trans-Atlantic journey. Scientists have not only measured the volume of dust, they have also calculated how much phosphorus – remnant in Saharan sands from part of the desert’s past as a lake bed – gets carried across the ocean from one of the planet’s most desolate places to one of its most fertile.

For the first time, a NASA satellite has quantified in three dimensions how much dust makes the trans-Atlantic journey from the Sahara Desert the Amazon rain forest. Among this dust is phosphorus, an essential nutrient that acts like a fertilizer, which the Amazon depends on in order to flourish. Image Credit: NASA’s Goddard Space Flight Center

A new paper published Feb. 24 in Geophysical Research Letters, a journal of the American Geophysical Union, provides the first satellite-based estimate of this phosphorus transport over multiple years, said lead author Hongbin Yu, an atmospheric scientist at the University of Maryland who works at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. A paper published online by Yu and colleagues Jan. 8 in Remote Sensing of the Environment provided the first multi-year satellite estimate of overall dust transport from the Sahara to the Amazon.

This trans-continental journey of dust is important because of what is in the dust, Yu said. Specifically the dust picked up from the Bodélé Depression in Chad, an ancient lake bed where rock minerals composed of dead microorganisms are loaded with phosphorus. Phosphorus is an essential nutrient for plant proteins and growth, which the Amazon rain forest depends on in order to flourish.

Nutrients – the same ones found in commercial fertilizers – are in short supply in Amazonian soils. Instead they are locked up in the plants themselves. Fallen, decomposing leaves and organic matter provide the majority of nutrients, which are rapidly absorbed by plants and trees after entering the soil. But some nutrients, including phosphorus, are washed away by rainfall into streams and rivers, draining from the Amazon basin like a slowly leaking bathtub.

The phosphorus that reaches Amazon soils from Saharan dust, an estimated 22,000 tons per year, is about the same amount as that lost from rain and flooding, Yu said. The finding is part of a bigger research effort to understand the role of dust and aerosols in the environment and on local and global climate.

Dust in the Wind

“We know that dust is very important in many ways. It is an essential component of the Earth system. Dust will affect climate and, at the same time, climate change will affect dust,” said Yu. To understand what those effects may be, “First we have to try to answer two basic questions. How much dust is transported? And what is the relationship between the amount of dust transport and climate indicators?”

The new dust transport estimates were derived from data collected by a lidar instrument on NASA’s Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation, or CALIPSO, satellite from 2007 though 2013.

sahara-dust-to-amazon_curtains[1]

The lidar instrument aboard the CALIPSO satellite sends out pulses of light that bounce off particles in the atmosphere and back to the satellite. It distinguishes dust from other particles based on optical properties. Image Credit: NASA Goddard’s Scientific Visualization Studio

The data show that wind and weather pick up on average 182 million tons of dust each year and carry it past the western edge of the Sahara at longitude 15W. This volume is the equivalent of 689,290 semi trucks filled with dust. The dust then travels 1,600 miles across the Atlantic Ocean, though some drops to the surface or is flushed from the sky by rain. Near the eastern coast of South America, at longitude 35W, 132 million tons remain in the air, and 27.7 million tons – enough to fill 104,908 semi trucks – fall to the surface over the Amazon basin. About 43 million tons of dust travel farther to settle out over the Caribbean Sea, past longitude 75W.

Yu and colleagues focused on the Saharan dust transport across the Atlantic Ocean to South America and then beyond to the Caribbean Sea because it is the largest transport of dust on the planet.

Dust collected from the Bodélé Depression and from ground stations on Barbados and in Miami give scientists an estimate of the proportion of phosphorus in Saharan dust. This estimate is used to calculate how much phosphorus gets deposited in the Amazon basin from this dust transport.

The seven-year data record, while too short for looking at long-term trends, is nevertheless very important for understanding how dust and other aerosols behave as they move across the ocean, said Chip Trepte, project scientist for CALIPSO at NASA’s Langley Research Center in Virginia, who was not involved in either study.

“We need a record of measurements to understand whether or not there is a fairly robust, fairly consistent pattern to this aerosol transport,” he said.

Looking at the data year by year shows that that pattern is actually highly variable. There was an 86 percent change between the highest amount of dust transported in 2007 and the lowest in 2011, Yu said.

Why so much variation? Scientists believe it has to do with the conditions in the Sahel, the long strip of semi-arid land on the southern border of the Sahara. After comparing the changes in dust transport to a variety of climate factors, the one Yu and his colleagues found a correlation to was the previous year’s Sahel rainfall. When Sahel rainfall increased, the next year’s dust transport was lower.

The mechanism behind the correlation is unknown, Yu said. One possibility is that increased rainfall means more vegetation and less soil exposed to wind erosion in the Sahel. A second, more likely explanation is that the amount of rainfall is related to the circulation of winds, which are what ultimately sweep dust from both the Sahel and Sahara into the upper atmosphere where it can survive the long journey across the ocean.

CALIPSO collects “curtains” of data that show valuable information about the altitude of dust layers in the atmosphere. Knowing the height at which dust travels is important for understanding, and eventually using computers to model, where that dust will go and how the dust will interact with Earth’s heat balance and clouds, now and in future climate scenarios.

“Wind currents are different at different altitudes,” said Trepte. “This is a step forward in providing the understanding of what dust transport looks like in three dimensions, and then comparing with these models that are being used for climate studies.”

Climate studies range in scope from global to regional changes, such as those that may occur in the Amazon in coming years. In addition to dust, the Amazon is home to many other types of aerosols like smoke from fires and biological particles, such as bacteria, fungi, pollen, and spores released by the plants themselves. In the future, Yu and his colleagues plan to explore the effects of those aerosols on local clouds – and how they are influenced by dust from Africa.

“This is a small world,” Yu said, “and we’re all connected together.”

NASA Terra satellite captures great image of Eastern US snow cover

Whole lotta snow is covering much of the USA. Check out this image of the northeastern quadrant of the country taken by NASA’s Terra satellite :

NASA Snaps Picture of Eastern U.S. in a Record-Breaking “Freezer”

unitedstates.a2015050.1620.1km[1]Click for large image.
NASA’s Terra satellite captured this picture of snow across the eastern

United States on Feb. 19 at 16:20 UTC (11:20 a.m. EST). 
Image Credit: NASA Goddard MODIS Rapid Response Team

NASA’s Terra satellite captured an image of the snow-covered eastern U.S. that looks like the states have been sitting in a freezer. In addition to the snow cover, Arctic and Siberian air masses have settled in over the Eastern U.S. triggering many record low temperatures in many states.

On Feb. 19 at 16:40 UTC (11:40 a.m. EST), the Moderate Resolution Imaging Spectroradiometer (MODIS) instrument that flies aboard NASA’s Terra satellite captured a picture of the snowy landscape. The snow cover combined with the frosty air mass made the eastern U.S. feel like the inside of freezer. The MODIS image was created at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.

On the morning of Feb. 20, NOAA’s Weather Prediction Center (WPC) noted, “There were widespread subzero overnight lows Thursday night (Feb. 19) extending from Illinois to western Virginia, and numerous record lows were set. Bitterly-cold arctic air is setting numerous temperature records across the eastern U.S. and will keep temperatures well below normal on Friday (Feb. 20).”

In Baltimore, Maryland, a low temperature of 1F broke the record low for coldest morning recorded at the Thurgood Marshall Baltimore Washington-International Airport.

In Louisville, Kentucky, temperatures dropped to -6F, breaking the old record low of 0F, according to meteorologist Brian Goode of WAVE-TV.  Meanwhile, Richmond Kentucky bottomed out at a frigid -32F.

In North Carolina, a record low temperature was set at Charlotte where the overnight temperature bottomed out at 7F breaking the old record of 13F in 1896. In Asheville, temperatures dropped to just 4F breaking the old record of 10F in 1979. Temperature records for Asheville extend back to 1876.

Several records were also broken in Georgia, according to Matt Daniel, a meteorologist at WMAZ-TV, Macon Georgia, who cited data from the National Weather Service. Daniel said that Macon set a new record low when the temperature dropped to 18F, beating the previous record of 21F set in 1958. Athens broke a new record low, too dropping to 14F and beating the old record of 18F set in 1958/1928.

NOAA’s NPC noted that “Highs on Friday (Feb. 20) will struggle to get out of the teens from the Ohio Valley to the Mid-Atlantic region.  After Friday, temperatures are forecast to moderate and get closer to February averages as a storm system approaches from the west.”

Rob Gutro 
NASA’s Goddard Space Flight Center