The Path To High Adventure Begins With Girl Scouting!

6 Ways NASA Space Communications Connect Astronauts to Earth

1. When Astronauts Phone Home, the Space Network Answers 

Operated by our Goddard Space Flight Center in Greenbelt, Maryland, this communications system enables all types of Earth-to-astronaut communication.  The Space Network is a complex system of ground station terminals and satellites. The satellites, called ‘Tracking and Data Relay Satellites’ or TDRS, provide continuous communications for human spaceflight 24/7/365. The information this network relays includes astronaut communication with Mission Control in Houston, posting live video of spacewalks and live interviews with schools, even posting Tweets on Twitter and doing Facebook posts. The Space Network can even broadcast live 4K, ultra-HD video right from the station. You can now watch an astronaut eat a space taco in high definition. WHAT A TIME TO BE ALIVE!

2. The Space Network Also Communicates Science Data 

Astronauts on the Space Station perform experiments on the station that will enable our Journey to Mars and other future human space missions. For example, astronaut Peggy Whitson works on a bone cell study that could lead to better preventative care or therapeutic treatments for people suffering bone loss as a result of bone diseases like osteopenia and osteoporosis, or for patients on prolonged bed rest. All that fantastic data is sent back to Earth via our Space Network for scientists around the world to analyze and build on.

3. The Space Network Transmits Spacecraft Health Data

The Space Network not only lets us communicate with the astronauts, it also tracks the ‘health’ of the spacecraft, be it the International Space Station where the astronauts are living, a cargo vehicle servicing the space station, or even, in the near future, crewed vehicles to other worlds. We deliver data on a spacecraft’s state of health, from power generation levels and avionics status to carbon dioxide and oxygen levels, and more to Mission Control 24/7/365.

4. The Space Network Helps Monitor Spacecraft Location

The International Space Station Is pretty big, but space is bigger. The Space Network enables flight controllers on the ground to provide a GPS-type service for the Space Station, letting them track the exact location of the space station at all times as it orbits the Earth. It also allows us Earth-bound folk to get real-time text updates when the Space Station is flying overhead. If you want to track the station, sign up here: https://spotthestation.nasa.gov

5. The Space Network Supports Launch Vehicles

Goddard’s Space Network also controls all the communications for all the missions that go to the space station. That includes command and telemetry services during launches, free flight, berthing and un-berthing to the station, as well as re-entry and landing back to Earth. 

6. The Space Network Is Also Looking Toward the Future

It’s also helping to test vehicles that will carry astronauts to other worlds. Currently, they are working with teams for our Space Launch System and commercial crew vehicles. The first flights for these vehicles will occur in 2018 and 2019, setting us on the road to Journey to Mars! This image shows the Orion capsule that will aid in our continuous march into space. 

What’s Next for the Space Network? 

We’re continuing to grow! Watch out for the launch of a new TDRS spacecraft in August 2017! TDRS-M is coming. Check out more info here and join our countdown to TDRS launch: https://tdrs.gsfc.nasa.gov. 

NASA Tech Launching on the Falcon Heavy

Later this month, a SpaceX Falcon Heavy rocket will take to the skies for the third time to launch the Department of Defense’s Space Test Program-2 (STP-2) mission. Several exciting, one-of-a-kind NASA technology and science payloads are among the two-dozen spacecraft aboard.

First, let’s talk about that Falcon Heavy rocket. Its 27 engines generate thrust at liftoff equal to that of approximately 18 airplanes, and it can lift over 140,000 pounds.

Managed by the U.S. Air Force Space and Missile Systems Center, STP-2 is the first government-contracted Falcon Heavy launch. It will reuse the two side boosters recovered after the April flight. SpaceX describes it as one of the most challenging launches in the company’s history.

It’s a big deal to us at NASA because we’re launching some pretty cool technologies. The tech will support our future exploration plans by helping improve future spacecraft design and performance. Here’s a bit about each:

Deep Space Atomic Clock

Time is the heartbeat of space navigation. Today, we navigate in deep space by using giant antennas on Earth to send signals to spacecraft, which then send those signals back to Earth. Atomic clocks on Earth measure the time it takes a signal to make this two-way journey. Only then can human navigators on Earth use large antennas to tell the spacecraft where it is and where to go.

Our Jet Propulsion Laboratory has been perfecting an atomic clock fit for exploration missions. The Deep Space Atomic Clock is the first atomic clock designed to fly on a spacecraft destined for beyond Earth's orbit. The timepiece is lighter and smaller—no larger than a toaster oven—than its refrigerator-sized, Earthly counterparts.

This miniaturized clock could enable one-way navigation: a spacecraft receives a signal from Earth and can determine its location immediately using its own, built-in navigation system. Even smaller versions of the clock are being investigated right now that could be used for the growing number of small to mid-size satellites. As we go forward to the Moon with the Artemis program, precise measurements of time are key to mission success.

The Deep Space Atomic Clock is the primary payload onboard the General Atomics Electromagnetic Systems Orbital Test Bed satellite and will perform a year-long demonstration in space.

Enhanced Tandem Beacon Experiment (E-TBEx)

Two tiny satellites will study how signals can be muddled as they travel through hard-to-predict bubbles in the upper atmosphere. Signals sent from satellites down to Earth (and vice versa) can be disrupted by structured bubbles that sometimes form in Earth's upper atmosphere. Because this region is affected both by weather on Earth and conditions in space, it's hard to predict just when these bubbles will form or how they'll mess with signals.

The E-TBEx CubeSats (short for Enhanced Tandem Beacon Experiment) will try to shed some light on that question. As these little satellites fly around Earth, they'll send radio signals (like the ones used by GPS) to receiving stations on the ground. Scientists will be able to look at the signals received and see if they were jumbled as they traveled through the upper atmosphere down to Earth — which will help us track when these bubbles are forming and how much they're interfering with our signals.

Green Propellant Infusion Mission (GPIM)

For decades, we have relied on a highly toxic spacecraft fuel called hydrazine. The Green Propellant Infusion Mission (GPIM) will lay the foundation to replace conventional chemical propulsion systems with a safer and more efficient alternative for next-generation spacecraft.

GPIM will demonstrate a new propellant in space for the first time. Concocted by the U.S. Air Force Research Laboratory, this innovative, “green” fuel—which actually has more of a peach hue—is expected to improve overall spacecraft performance due to its higher density, increased thrust and lower freezing point in comparison with hydrazine.

GPIM’s propulsion system, developed by Aerojet Rocketdyne, consists of new compatible tanks, valves and thrusters. During the two-month-long demonstration on a Ball Aerospace spacecraft, engineers will conduct orbital maneuvers to demonstrate the performance of the propellant and propulsion system.

Space Environment Testbeds (SET)

It’s not easy being a spacecraft; invisible, energetic particles zip throughout space — and while there are so few that space is considered a vacuum, what’s there still packs a punch. Tiny particles — like those seen here impacting a detector on a Sun-studying spacecraft — can wreak havoc with the electronics we send up into space.

Space Environment Testbeds — or SET, for short — is a mission to study space radiation and how it affects spacecraft and electronics in orbit. What looks like snow flurries in these animated images, for example, is actually a solar radiation storm of incredibly fast particles, unleashed by a solar eruption. Energetic particles from the Sun or deep space can spark memory damage or computer upsets on spacecraft, and over time, degrade hardware.

By studying radiation effects and different methods to protect satellites, SET will help future missions improve spacecraft design, engineering and operations.

Follow @NASA_Technology and @NASASun on Twitter for news about the STP-2 launch and our missions aboard.

Check out www.nasa.gov/spacex to stay up-to-date on the launch day and time. Don’t forget to tune into our launch coverage, scheduled to start about 30 minutes before liftoff!

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Pinpointing the Cause of Earth’s Recent Record CO2 Spike

A new NASA study provides space-based evidence that Earth’s tropical regions were the cause of the largest annual increases in atmospheric carbon dioxide concentration seen in at least 2,000 years.

What was the cause of this?

Scientists suspect that the 2015-2016 El Niño – one of the largest on record – was responsible. El Niño is a cyclical warming pattern of ocean circulation in the Pacific Ocean that affects weather all over the world. Before OCO-2, we didn’t have enough data to understand exactly how El Nino played a part.

Analyzing the first 28 months of data from our Orbiting Carbon Observatory (OCO-2) satellite, researchers conclude that impacts of El Niño-related heat and drought occurring in the tropical regions of South America, Africa and Indonesia were responsible for the record spike in global carbon dioxide.

These three tropical regions released 2.5 gigatons more carbon into the atmosphere than they did in 2011. This extra carbon dioxide explains the difference in atmospheric carbon dioxide growth rates between 2011 and the peak years of 2015-16.

In 2015 and 2016, OCO-2 recorded atmospheric carbon dioxide increases that were 50% larger than the average increase seen in recent years preceding these observations.

In eastern and southern tropical South America, including the Amazon rainforest, severe drought spurred by El Niño made 2015 the driest year in the past 30 years. Temperatures were also higher than normal. These drier and hotter conditions stressed vegetation and reduced photosynthesis, meaning trees and plants absorbed less carbon from the atmosphere. The effect was to increase the net amount of carbon released into the atmosphere.

In contrast, rainfall in tropical Africa was at normal levels, but ecosystems endured hotter-than-normal temperatures. Dead trees and plants decomposed more, resulting in more carbon being released into the atmosphere.

Meanwhile, tropical Asia had the second-driest year in the past 30 years. Its increased carbon release, primarily from Indonesia, was mainly due to increased peat and forest fires -  also measured by satellites.

We knew El Niños were one factor in these variations, but until now we didn’t understand, at the scale of these regions, what the most important processes were. OCO-2’s geographic coverage and data density are allowing us to study each region separately.

Why does the amount of carbon dioxide in our atmosphere matter?

The concentration of carbon dioxide in Earth’s atmosphere is constantly changing. It changes from season to season as plants grow and die, with higher concentrations in the winter and lower amounts in the summer. Annually averaged atmospheric carbon dioxide concentrations have generally increased year over year since the 1800s – the start of the widespread Industrial Revolution. Before then, Earth’s atmosphere naturally contained about 595 gigatons of carbon in the form of carbon dioxide. Currently, that number is 850 gigatons.

Carbon dioxide is a greenhouse gas, which means that it can trap heat. Since greenhouse gas is the principal human-produced driver of climate change, better understanding how it moves through the Earth system at regional scales and how it changes over time are important aspects to monitor.

Get more information about these data HERE.

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Is the earth really as beautiful as they say from space?

What is a Supermoon Lunar Eclipse?

We’ve told you that on Sept. 27 a supermoon lunar eclipse will occur in the U.S. And much of the world, but what does that mean?

One important note, is that this event can be referred to in many different ways: 

Supermoon Lunar Eclipse

Super Blood Moon

Harvest Moon Eclipse

Supermoon Eclipse

All slightly different names, but apply to the same spectacular event that will occur this weekend. 

Since it’s rare that both a supermoon and an lunar eclipse occur at the same time, let’s break it down. 

1) Supermoon

A supermoon is a full or new moon that falls closest to the fall equinox, and is at its closest approach to the Earth. This results in the moon appearing up to 14% larger in diameter.

2) Lunar Eclipse 

A lunar eclipse occurs when the moon passes directly behind the Earth into its shadow. This can give the moon a red tint.

3) A Supermoon Lunar Eclipse!

The combination of these two events does not happen very often. In fact, since 1900 a supermoon lunar eclipse has only happened 5 times! The last time this occurred was 1982, and if you miss the event this year, your next opportunity won’t come until 2033.

This year, the event will be visible from the Americas, Europe and Africa on the night of Sept. 27. Here’s a full schedule of the supermoon eclipse:

If it’s cloudy in your area on Sept. 27, don’t worry! NASA Television will be providing a live stream of the event, so you can tune in and enjoy the show. 

For more information and resources on the supermoon lunar eclipse, visit our page on NASA.gov.

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10 People You Wish You Met from 100 Years of NASA’s Langley

Something happened 100 years ago that changed forever the way we fly. And then the way we explore space. And then how we study our home planet. That something was the establishment of what is now NASA Langley Research Center in Hampton, Virginia. Founded just three months after America's entry into World War I, Langley Memorial Aeronautical Laboratory was established as the nation's first civilian facility focused on aeronautical research. The goal was, simply, to "solve the fundamental problems of flight."

From the beginning, Langley engineers devised technologies for safer, higher, farther and faster air travel. Top-tier talent was hired. State-of-the-art wind tunnels and supporting infrastructure was built. Unique solutions were found.

Langley researchers developed the wing shapes still used today in airplane design. Better propellers, engine cowlings, all-metal airplanes, new kinds of rotorcraft and helicopters, faster-than-sound flight - these were among Langley's many groundbreaking aeronautical advances spanning its first decades.

By 1958, Langley's governing organization, the National Advisory Committee for Aeronautics, or NACA, would become NASA, and Langley's accomplishments would soar from air into space.

Here are 10 people you wish you met from the storied history of Langley:

Robert R. "Bob" Gilruth (1913–2000) 

Considered the father of the U.S. manned space program.

He helped organize the Manned Spacecraft Center – now the Johnson Space Center – in Houston, Texas. 

Gilruth managed 25 crewed spaceflights, including Alan Shepard's first Mercury flight in May 1961, the first lunar landing by Apollo 11 in July 1969, the dramatic rescue of Apollo 13 in 1970, and the Apollo 15 mission in July 1971.

Christopher C. "Chris" Kraft, Jr. (1924-) 

Created the concept and developed the organization, operational procedures and culture of NASA’s Mission Control.

Played a vital role in the success of the final Apollo missions, the first manned space station (Skylab), the first international space docking (Apollo-Soyuz Test Project), and the first space shuttle flights.

Maxime "Max" A. Faget (1921–2004) 

Devised many of the design concepts incorporated into all U.S.  manned spacecraft.

The author of papers and books that laid the engineering foundations for methods, procedures and approaches to spaceflight. 

An expert in safe atmospheric reentry, he developed the capsule design and operational plan for Project Mercury, and made major contributions to the Apollo Program’s basic command module configuration.

Caldwell Johnson (1919–2013) 

Worked for decades with Max Faget helping to design the earliest experimental spacecraft, addressing issues such as bodily restraint and mobility, personal hygiene, weight limits, and food and water supply. 

A key member of NASA’s spacecraft design team, Johnson established the basic layout and physical contours of America’s space capsules.

William H. “Hewitt” Phillips (1918–2009) 

Provided solutions to critical issues and problems associated with control of aircraft and spacecraft. 

Under his leadership, NASA Langley developed piloted astronaut simulators, ensuring the success of the Gemini and Apollo missions. Phillips personally conceived and successfully advocated for the 240-foot-high Langley Lunar Landing Facility used for moon-landing training, and later contributed to space shuttle development, Orion spacecraft splashdown capabilities and commercial crew programs.

Katherine Johnson (1918-) 

Was one of NASA Langley’s most notable “human computers,” calculating the trajectory analysis for Alan Shepard’s May 1961 mission, Freedom 7, America’s first human spaceflight. 

She verified the orbital equations controlling the capsule trajectory of John Glenn’s Friendship 7 mission from blastoff to splashdown, calculations that would help to sync Project Apollo’s lunar lander with the moon-orbiting command and service module. 

Johnson also worked on the space shuttle and the Earth Resources Satellite, and authored or coauthored 26 research reports.

Dorothy Vaughan (1910–2008) 

Was both a respected mathematician and NASA's first African-American manager, head of NASA Langley’s segregated West Area Computing Unit from 1949 until 1958. 

Once segregated facilities were abolished, she joined a racially and gender-integrated group on the frontier of electronic computing. 

Vaughan became an expert FORTRAN programmer, and contributed to the Scout Launch Vehicle Program.

William E. Stoney Jr. (1925-) 

Oversaw the development of early rockets, and was manager of a NASA Langley-based project that created the Scout solid-propellant rocket. 

One of the most successful boosters in NASA history, Scout and its payloads led to critical advancements in atmospheric and space science. 

Stoney became chief of advanced space vehicle concepts at NASA headquarters in Washington, headed the advanced spacecraft technology division at the Manned Spacecraft Center in Houston, and was engineering director of the Apollo Program Office.

Israel Taback (1920–2008) 

Was chief engineer for NASA’s Lunar Orbiter program. Five Lunar Orbiters circled the moon, three taking photographs of potential Apollo landing sites and two mapping 99 percent of the lunar surface. 

Taback later became deputy project manager for the Mars Viking project. Seven years to the day of the first moon landing, on July 20, 1976, Viking 1 became NASA’s first Martian lander, touching down without incident in western Chryse Planitia in the planet’s northern equatorial region.

John C Houbolt (1919–2014) 

Forcefully advocated for the lunar-orbit-rendezvous concept that proved the vital link in the nation’s successful Apollo moon landing. 

In 1963, after the lunar-orbit-rendezvous technique was adopted, Houbolt left NASA for the private sector as an aeronautics, astronautics and advanced-technology consultant. 

He returned to Langley in 1976 to become its chief aeronautical scientist. During a decades-long career, Houbolt was the author of more than 120 technical publications.

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What are Phytoplankton and Why Are They Important?

Breathe deep… and thank phytoplankton.

Why? Like plants on land, these microscopic creatures capture energy from the sun and carbon from the atmosphere to produce oxygen.

Phytoplankton are microscopic organisms that live in watery environments, both salty and fresh. Though tiny, these creatures are the foundation of the aquatic food chain. They not only sustain healthy aquatic ecosystems, they also provide important clues on climate change.

Let’s explore what these creatures are and why they are important for NASA research.

Phytoplankton are diverse

Phytoplankton are an extremely diversified group of organisms, varying from photosynthesizing bacteria, e.g. cyanobacteria, to diatoms, to chalk-coated coccolithophores. Studying this incredibly diverse group is key to understanding the health - and future - of our ocean and life on earth.

Their growth depends on the availability of carbon dioxide, sunlight and nutrients. Like land plants, these creatures require nutrients such as nitrate, phosphate, silicate, and calcium at various levels. When conditions are right, populations can grow explosively, a phenomenon known as a bloom.

Phytoplankton blooms in the South Pacific Ocean with sediment re-suspended from the ocean floor by waves and tides along much of the New Zealand coastline.

Phytoplankton are Foundational

Phytoplankton are the foundation of the aquatic food web, feeding everything from microscopic, animal-like zooplankton to multi-ton whales. Certain species of phytoplankton produce powerful biotoxins that can kill marine life and people who eat contaminated seafood.

Phytoplankton are Part of the Carbon Cycle

Phytoplankton play an important part in the flow of carbon dioxide from the atmosphere into the ocean. Carbon dioxide is consumed during photosynthesis, with carbon being incorporated in the phytoplankton, and as phytoplankton sink a portion of that carbon makes its way into the deep ocean (far away from the atmosphere).

Changes in the growth of phytoplankton may affect atmospheric carbon dioxide concentrations, which impact climate and global surface temperatures. NASA field campaigns like EXPORTS are helping to understand the ocean's impact in terms of storing carbon dioxide.

Phytoplankton are Key to Understanding a Changing Ocean

NASA studies phytoplankton in different ways with satellites, instruments, and ships. Upcoming missions like Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) - set to launch Jan. 2024 - will reveal interactions between the ocean and atmosphere. This includes how they exchange carbon dioxide and how atmospheric aerosols might fuel phytoplankton growth in the ocean.

Information collected by PACE, especially about changes in plankton populations, will be available to researchers all over the world. See how this data will be used.

The Ocean Color Instrument (OCI) is integrated onto the PACE spacecraft in the cleanroom at Goddard Space Flight Center. Credit: NASA

We’re On a Mission to Study The Zone Where Earth Meets Space!

We’re launching ICON — short for Ionospheric Connection Explorer — a mission to explore the dynamic region where Earth meets space: the ionosphere!

Earth’s ionosphere stretches from 50 to 400 miles above the ground, overlapping the top of our atmosphere and the very beginning of space. The Sun cooks gases there until they lose an electron (or two or three), creating a sea of electrically charged particles. But, the ionosphere also responds to weather patterns from Earth rippling up. These changes are complex and tricky to understand.

That’s why we’re launching ICON! Changes in the ionosphere can affect astronauts, satellites and communications signals we use every day, like radio or GPS. Understanding these changes could help us eventually predict them — and better protect our technology and explorers in space.

ICON will track changes in the ionosphere by surveying airglow. It’s a natural feature of Earth’s that causes our atmosphere to constantly glow. The Sun excites gases in the upper atmosphere, so they emit light. From 360 miles above Earth, ICON will photograph airglow to measure the ionosphere’s winds, composition and temperature. ICON also carries an instrument that will capture and measure the particles directly around the spacecraft.

ICON is scheduled to launch on Oct. 10, on a Northrop Grumman Pegasus XL rocket. The night of launch, the rocket is flown up to the sky by Northrop Grumman’s L-1011 Stargazer airplane, which takes off from Cape Canaveral Air Force Station in Florida. From 40,000 feet above the open ocean, the Pegasus XL rocket drops from the plane and free-falls for about five seconds before igniting and carrying ICON into orbit.   

NASA TV coverage of the launch starts at 9:15 p.m. EDT on Oct. 10 at nasa.gov/live. You can also follow along on Twitter, Facebook or at nasa.gov/icon.

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Greenland Refrozen

It won’t be until summertime that a significant amount of melt shows up across the Greenland Ice Sheet. For now, most indications of meltwater ponds and lakes are leftovers from past seasons that have since refrozen.

These photographs were snapped during research flights for NASA’s Operation IceBridge—now in its final year after a decade of airborne missions to map polar ice.

This second image was acquired on April 18, 2019, with the Continuous Airborne Mapping by Optical Translator (CAMBOT) system. The system takes downward-looking images throughout a flight, which can later be used by scientists to interpret other data. This image shows part of a large, frozen lake on Storstrømmen Glacier. This lake also thaws in summertime, which is why it shows up as blue ice.

Lakes atop a glacier, or “supraglacial lakes,” are somewhat stable in terms of their location, according to Joe MacGregor, NASA project scientist for Operation IceBridge. The lake on Storstrømmen is visible in satellite data at least as far back as May 2012. On occasion, water in lakes like this can drain away through a vertical shaft known as a “moulin.” Scientists initially wondered if the dark circular area on the right side of this image could be a moulin, but closer inspection suggested it is just a deeper part of the lake.

See more photos of the frozen lakes in Greenland: https://earthobservatory.nasa.gov/images/144965/greenland-refrozen

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Help us put the ART in Artemis! Our step-by-step draw Artemis guide will help you learn how to draw the space suit that will keep our astronauts safe during their trip to the Moon.  Have fun, get creative and share your drawings using the hashtag #drawArtemis! 

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Do illustrations suit you? Then enjoy NASA at Home fun while learning to draw Orion’s Space Suit that will keep Astronauts safe during Artemis missions to the Moon! Visit https://go.nasa.gov/2SRacx2 for instructions and be sure to share your tailor-made suits to #drawARTEMIS