Currently, six humans are living and working on the International Space Station, which orbits 250 miles above our planet at 17,500mph. Below you will find a real journal entry, written in space, by NASA astronaut Scott Tingle.
To read more entires from this series, visit our Space Blogs on Tumblr.
I did an interview with some students today, and I was asked a two-part question by one of the students. He asked, “What is the most exciting thing about being in space, and how did you keep yourself motivated to get there?”
I answered, “When you were very young, did you ever dream or wish you could fly? We all know it’s impossible, right? Imagine waking up one day and finding out you actually can fly! THAT is exciting! Now consider the contrary thought, what if you grew up and realized that flying wasn’t possible for humans, and you were at peace with this reality, and at peace shedding your childhood dream of flying? You will have several crossroads in your life, and you will have to decide which of these people you want to be. I too am amazed that I had the staying power to continue to dream as I did when I was a child. Words cannot describe how I feel when I fly through the International Space Station every day.”
Find more ‘Captain’s Log’ entries HERE.
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In late December 2014, an underwater volcano in the South Pacific Kingdom of Tonga erupted and sent a violent stream of steam, ash and rock into the air. The ash plumes rose as high as 30,000 feet (9 kilometers) into the sky and diverted airline flights.
Most new oceanic islands often wash away quickly within a few months. The island doesn't have an official name, and is referred to as Hunga Tonga-Hunga Ha'apai after two older islands to either side.
But this island was different. One of our satellites that detects volcanic eruptions alerted our scientists who were very excited because this type of explosive, undersea eruption is rare. In fact, the new Tongan island is one of only three of this kind of volcanic islands in the past 150 years to emerge and survive. It's now three years old.
The baby island is also the first of its kind to emerge in the modern satellite era. This is really important since it's difficult to send our researchers the South Pacific every month to see how the island has changed – which it did very rapidly, especially in the first six months. But satellites in space delivered monthly views which we used to make these high resolution, 3-D topographic maps. With these maps, we tracked the early life and evolution of the island in unprecedented detail.
In April 2015, we watched an isthmus bridge begin forming from the new island to the older island neighboring it to the east. Soft volcanic material, especially on the island's southern side, was eroded by the ocean and deposited on the tail end, which grew and grew till it reached the other island. It's about 1600 feet (500 meters) across, or the length of 5 football fields.
The erosive forces of the ocean broke down the southern wall of the crater lake in May 2015. We thought this might mean that the island wouldn't last much longer because the ocean could now attack the interior of the island's tuff cone. But in June, a sandbar formed, closing off the lake again and protecting the interior. The sandbar has been in place ever since.
Monitoring these changes of both erosion and growth, we now believe that the island will last from between 6 to 30 years!
Why has the island survived for three years? What makes eroding it away harder than for other blink-and-you-miss-it oceanic islands that disappear into the sea after a few months? To answer these questions, we need rock samples.
Working with the Tongan government, we recruited two French citizens sailing around the world who were in Tongan waters in June, 2017, to go to the new island on our behalf. We treated them like astronauts and gave them instructions to take pictures and samples of the volcanic rocks at locations we could see from space along the coasts, the interior of the crater lake, and from the top of the tuff cone.
They did a fantastic job documenting each sample and where it came from, and then mailed the box of rocks back to our team at our Goddard Space Flight Center in Greenbelt, Maryland, where they are currently being analyzed. We believe that after the eruption, warm seawater mixed with volcanic ash to chemically alter it so that when it hardened into rock it was a tougher material. We're excited to see if the rock samples confirm this.
Link: https://svs.gsfc.nasa.gov/11372
Did these Martian volcanoes form in an ocean or lake? If they did, wet environments such as these combined with heat from volcanic processes may be prime locations to search for evidence of past life. We may not know until we arrive on the red planet, but by studying Earth's landforms, we'll be better prepared when we do.
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The Aral Sea was once the fourth-largest lake in the world. Fed primarily by snowmelt and precipitation flowing down from faraway mountains, it was a temperate oasis in an arid region. But in the 1960s, the Soviet Union diverted two major rivers to irrigate farmland, cutting off the inland sea from its source. As the Aral Sea dried up, fisheries collapsed, as did the communities that depended on them. The remaining water supply became increasingly salty and polluted with runoff from agricultural plots. Loss of the Aral Sea's water influenced regional climate, making the winters even colder and the summers much hotter.
While seasonal rains still bring water to the Aral Sea, the lake is roughly one-tenth of its original size. These satellite images show how the Aral Sea and its surrounding landscape has changed over the past few decades.
For more details about these images, read the full stories here: https://go.nasa.gov/2PqJ1ot
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For decades, astronomers searched the cosmos for what is thought to be the first kind of molecule to have formed after the Big Bang. Now, it has finally been found. The molecule is called helium hydride. It’s made of a combination of hydrogen and helium. Astronomers think the molecule appeared more than 13 billion years ago and was the beginning step in the evolution of the universe. Only a few kinds of atoms existed when the universe was very young. Over time, the universe transformed from a primordial soup of simple molecules to the complex place it is today — filled with a seemingly infinite number of planets, stars and galaxies. Using SOFIA, the world’s largest airborne observatory, scientists detected newly formed helium hydride in a planetary nebula 3,000 light-years away. It was the first ever detection of the molecule in the modern universe. Learn more about the discovery:
The discovery serves as proof that helium hydride can, in fact, exist in space. This confirms a key part of our basic understanding of the chemistry of the early universe. SOFIA is a modified Boeing 747SP aircraft that allows astronomers to study the solar system and beyond in ways that are not possible with ground-based telescopes. Find out more about the mission at www.nasa.gov/SOFIA
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For the first time, measurements from our Earth-observing satellites are being used to help combat a potential outbreak of life-threatening cholera. Humanitarian teams in Yemen are targeting areas identified by a NASA-supported project that precisely forecasts high-risk regions based on environmental conditions observed from space.
Cholera is caused by consuming food or water contaminated with a bacterium called Vibrio cholerae.
The disease affects millions of people every year and can be deadly. It remains a major threat to global health, especially in developing countries, such as Yemen, where access to clean water is limited.
To calculate the likelihood of an outbreak, scientists run a computer model that takes satellite observations of things like rain and temperatures and combines them with information on local sanitation and clean water infrastructure. In 2017, the model achieved 92 percent accuracy in predicting the regions where cholera was most likely to occur and spread in Yemen. An outbreak that year in Yemen was the world's worst, with more than 1.1 million suspected cases and more than 2,300 deaths, according to the World Health Organization.
International humanitarian organizations took notice. In January 2018, Fergus McBean, a humanitarian adviser with the U.K.'s Department for International Development, read about the NASA-funded team's 2017 results and contacted them with an ambitious challenge: to create and implement a cholera forecasting system for Yemen, in only four months.
“It was a race against the start of rainy season,” McBean said.
The U.S. researchers began working with U.K. Aid, the U.K. Met Office, and UNICEF on the innovative approach to use the model to inform cholera risk reduction in Yemen.
In March, one month ahead of the rainy season, the U.K. international development office began using the model’s forecasts. Early results show the science team’s model predictions, coupled with Met Office weather forecasts, are helping UNICEF and other aid groups target their response to where support is needed most.
Photo Credit: UNICEF
“By joining up international expertise with those working on the ground, we have for the very first time used these sophisticated predictions to help save lives and prevent needless suffering,” said Charlotte Watts, chief scientist for United Kingdom’s Department for International Development.
Read more: go.nasa.gov/2MxKyw4
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If I am in the path of totality (Hopkinsville, KY) when can I take off my glasses to view the eclipse? Can I keep them off for the entire 2 minutes and 40 seconds?
If you are viewing the partial eclipse or lead up to totality, once you no longer can see any light through your eclipse glasses, then you can take them off. As long as the moon is fully covering the Sun you are safe. I would err on the side of caution and look away from the Sun a few moments before it’s over. This is also a great time to see what is happening around you! The animals should be responding differently than normal and this would be a great time to see that.
New science is headed to the International Space Station aboard the SpaceX Dragon.
Investigations on this flight include a test of robotic technology for refueling spacecraft, a project to map the world’s forests and two student studies inspired by Marvel’s “Guardians of the Galaxy” series.
Learn more about the science heading into low-Earth orbit:
The Global Ecosystem Dynamics Investigation (GEDI) is an instrument to measure and map Earth’s tropical and temperate forests in 3D.
The Jedi knights may help protect a galaxy far, far away, but our GEDI will help us study and understand forest changes right here on Earth.
What’s cooler than cool? Cryogenic propellants, or ice-cold spacecraft fuel! Our Robotic Refueling Mission 3 (RRM3) will demonstrate technologies for storing and transferring these special liquids. By establishing ways to replenish this fuel supply in space, RRM3 could help spacecraft live longer and journey farther.
The mission’s techniques could even be applied to potential lunar gas stations at the Moon, or refueling rockets departing from Mars.
The Molecular Muscle investigation examines the molecular causes of muscle abnormalities from spaceflight in C. elgans, a roundworm and model organism.
This study could give researchers a better understanding of why muscles deteriorate in microgravity so they can improve methods to help crew members maintain their strength in space.
Perfect Crystals is a study to learn more about an antioxidant protein called manganese superoxide dismutase that protects the body from the effects of radiation and some harmful chemicals.
The station’s microgravity environment allows researchers to grow more perfectly ordered crystals of the proteins. These crystals are brought back to Earth and studied in detail to learn more about how the manganese superoxide dismutase works. Understanding how this protein functions may aid researchers in developing techniques to reduce the threat of radiation exposure to astronauts as well as prevent and treat some kinds of cancers on Earth.
SlingShot is a new, cost-effective commercial satellite deployment system that will be tested for the first time.
SlingShot hardware, two small CubeSats, and a hosted payload will be carried to the station inside SpaceX’s Dragon capsule and installed on a Cygnus spacecraft already docked to the orbiting laboratory. Later, Cygnus will depart station and fly to a pre-determined altitude to release the satellites and interact with the hosted payload.
Spaceflight appears to accelerate aging in both humans and mice. Rodent Research-8 (RR-8) is a study to understand the physiology of aging and the role it plays on the progression of disease in humans. This investigation could provide a better understanding of how aging changes the body, which may lead to new therapies for related conditions experienced by astronauts in space and people on Earth.
The MARVEL ‘Guardians of the Galaxy’ Space Station Challenge is a joint project between the U.S. National Laboratory and Marvel Entertainment featuring two winning experiments from a contest for American teenage students. For the contest, students were asked to submit microgravity experiment concepts that related to the Rocket and Groot characters from Marvel’s “Guardians of the Galaxy” comic book series.
Team Rocket: Staying Healthy in Space
If an astronaut suffers a broken tooth or lost filling in space, they need a reliable and easy way to fix it. This experiment investigates how well a dental glue activated by ultraviolet light would work in microgravity. Researchers will evaluate the use of the glue by treating simulated broken teeth and testing them aboard the station.
Team Groot: Aeroponic Farming in Microgravity
This experiment explores an alternative method for watering plants in the absence of gravity using a misting device to deliver water to the plant roots and an air pump to blow excess water away. Results from this experiment may enable humans to grow fruits and vegetables in microgravity, and eliminate a major obstacle for long-term spaceflight.
These investigation join hundreds of others currently happening aboard the station. For more info, follow @ISS_Research!
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The United States has nearly 84 million acres of historic and scenic land in its national parks system. In celebration of National Park Week, here are some satellite views of a few of those national treasures.
Throughout National Park Week, you can #FindYourPark and visit for free.
Yosemite National Park – California
Naked summits alternate with forested lowlands in Yosemite Valley, part of California’s Yosemite National Park. Our Landsat 7 satellite captured this true-color image of part of the Yosemite Valley on Aug. 8, 2001.
Yellowstone National Park – Wyoming, Idaho and Montana
Established in 1872, it was the first national park in the United States, and the world! Its geological and biological wonders have led international groups to declare it a world heritage site and a biosphere reserve. Yellowstone National Park captures the spirit and purpose of the National Park Service, blending modern and ancient human history with nature in its raw complexity.
Hot Springs National Park – Arkansas
National Parks usually make us think of pristine landscapes untouched by human civilization. Most of the 59 national parks in the United States fit that mold, but there are a few exceptions. Arkansas’s Hot Springs National Park, the country’s smallest and most urban, is one of them. Hot Springs, a city of 96,000 people, lies at the southern edge of the park and partly within its boarders.
Shenandoah National Park – Virginia
This long, narrow park in the Blue Ridge Mountains spans more than 179,000 acres, with 40% of the land protected as wilderness. More than 95% of the park is forested, sheltering 1,300 plant species and 267 types of trees and shrubs. The park contains 577 archeological sites, more than 100 cemeteries, and some rocks that date back a billion years.
Olympic National Park – Washington
Possibly one of America’s most diverse national landscapes, Olympic National Park is situated on the Olympic Peninsula in northwestern Washington. If you walked from west to east across the park, you would start at the rocky Pacific shoreline, move into rare temperate rainforests and lush river valleys, ascend glaciers and rugged mountain peaks, and then descend into a comparatively dry rain shadow and alpine forest. From beach to the top of Mount Olympus, you would rise 7,980 feet above sea level.
Colorado National Monument – Colorado
Along the Interstate 70 corridor in western Colorado, well-watered croplands, residential properties and urbanized areas create a broad stripe of green and gray. Away from the interstate, dry climate conditions color the landscape shades of beige, brick and tan. Yet these arid regions offer treasures of their own, including stunning vistas and wildlife both living and extinct. The varied landscapes of this park show the effects of tens of millions of years of erosion.
The images above were produced by our Earth Observatory as part of its 2016 series featuring the National Park Service properties. Check out more HERE.
Want to see more of our nation’s parks from space? Visit our Flickr gallery HERE.
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Why are we studying them? What’s purpose of this field for us on earth?
Black holes are mystifying yet terrifying cosmic phenomena. Unfortunately, people have a lot of ideas about them that are more science fiction than science. Don’t worry! Our black hole expert, Jeremy Schnittman, will be answering your your questions in an Answer Time session on Wednesday, October 2 from 3pm - 4 pm ET here on NASA’s Tumblr! Make sure to ask your question now by visiting http://nasa.tumblr.com/ask!
Jeremy joined the Astrophysics Science Division at our Goddard Space Flight Center in 2010 following postdoctoral fellowships at the University of Maryland and Johns Hopkins University. His research interests include theoretical and computational modeling of black hole accretion flows, X-ray polarimetry, black hole binaries, gravitational wave sources, gravitational microlensing, dark matter annihilation, planetary dynamics, resonance dynamics and exoplanet atmospheres. He has been described as a "general-purpose astrophysics theorist," which he regards as quite a compliment.
Fun Fact: The computer code Jeremy used to make the black hole animations we featured last week is called "Pandurata," after a species of black orchid from Sumatra. The name pays homage to the laser fusion lab at the University of Rochester where Jeremy worked as a high school student and wrote his first computer code, "Buttercup." All the simulation codes at the lab are named after flowers.
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We're launching a new mission to the International Space Station to continue measurements of the Sun's energy reaching Earth.
The Total and Spectral solar Irradiance Sensor (TSIS-1) will precisely measure the total amount of sunlight that falls on Earth and how that light is distributed among different wavelengths, including the ultraviolet, visible and infrared. This will give us a better understanding of Earth’s primary energy supply and help improve models simulating Earth’s climate.
The Sun is Earth's sunshine and it does more than make us happy; it gives us life. Our Sun's energy drives our planet's ocean currents, seasons, weather and climate. Changes in the Sun also alter our climate in at least two ways.
First, solar radiation has a direct effect where it heats regions of Earth, like our oceans, land, and atmosphere. Second, the solar radiation can cause indirect effects, such as when sunlight interacts with molecules in the upper atmosphere to produce ozone which can affect human health.
Earth’s energy system is in a constant dance to maintain a balance between incoming energy from the Sun and outgoing energy from Earth to space, which scientists call Earth’s energy budget. If you have more energy absorbed by the Earth than leaving it, its temperature increases and vice versa. Because the Sun is Earth's fundamental energy source and only sunshine, we need a quantitative record of the Sun's solar energy output. TSIS-1 will provide the most accurate measurements ever made of sunlight as seen from above Earth’s atmosphere.
The energy flow between the Earth and Sun's connection is not a constant thing. The Sun can be fickle, sometimes it puts out slightly more energy and some years less. Earth is no better. The Earth absorbs different amounts of the Sun's energy depending on many factors, such as the presence of clouds and tiny particles in the atmosphere called aerosols.
What we do know is that the Sun's cycle is about 11 years rolling through periods of quiet to times of intense activity. When the Sun is super-intense it releases explosions of light and solar material. This time is a solar maximum.
When the Sun is in a quiet state this period is called the solar minimum.
Over the course of one solar cycle (one 11-year period), the Sun’s total emitted energy varies on average at about 0.1 percent. That may not sound like a lot, but the Sun emits a large amount of energy – 1,361 watts per square meter. Even fluctuations at just a tenth of a percent can affect Earth. That's why TSIS-1 is launching: to help scientists understand and anticipate how changes in the Sun will affect us on Earth.
Scientists use computer models to interpret changes in the Sun’s energy input. If less solar energy is available, scientists can gauge how that affects Earth’s atmosphere, oceans, weather and seasons by using computer simulations. But the Sun is just one of many factors scientists use to model Earth’s climate. A lot of other factors come into play in addition to the energy from the Sun. Factors like greenhouse gases, clouds scattering light and small particles in the atmosphere called aerosols all can affect Earth’s climate so they all need to be included in climate models. So, while we need to measure the total amount of energy from the Sun, we also need to understand how these other factors alter the amount of energy reaching Earth's surface and affect our climate.
We receive the Sun's energy in many different wavelengths, including visible light (rainbows!) as well as light we can't see like infrared and ultraviolet wavelengths. Each color or wavelength of light from the Sun affects Earth’s atmosphere differently.
For instance, ultraviolet light from the Sun can affect Earth's ozone. High in the atmosphere is a layer of protective ozone gas. Ozone is Earth’s natural sunscreen, absorbing the Sun’s most harmful ultraviolet radiation and protecting living things below. But ozone is vulnerable to certain gases made by humans that reach the upper atmosphere. Once there, they react in the presence of sunlight to destroy ozone molecules. Currently, several satellites from us and the National Oceanic and Atmospheric Administration (NOAA) track the ozone in the upper atmosphere and the solar energy that drives the photochemistry that creates and destroys ozone. Our new instrument, TSIS-1, will join that fleet with even better accuracy.
TSIS-1 will see different types of ultraviolet (UV) light, including UV-B and UV-C. Each plays a different role in the ozone layer. UV-C rays are essential in creating ozone. UV-B rays and some naturally occurring chemicals regulate the abundance of ozone in the upper atmosphere. The amount of ozone is a balance between these natural production and loss processes.
TSIS-1 data of the Sun's UV energy will help improve computer models of the atmosphere that need accurate measurements of sunlight across the ultraviolet spectrum to model the ozone layer correctly. While UV light represents a tiny fraction of the total sunlight that reaches the top of Earth's atmosphere, it fluctuates from 3 to 10 percent, a change that, in turn causes small changes in the chemical composition and thermal structure of the upper atmosphere.
This is just one of the important applications of TSIS-1 measurements. TSIS-1 will measure how the Sun's energy is distributed over 1,000 different wavelengths.
TSIS-1 will continue our nearly 40 years of closely studying the total amount of energy the Sun sends to Earth from space. We've previously studied this 'total solar irradiance' with nine previous satellites, currently with Solar Radiation and Climate Experiment, (SORCE).
NASA’s SORCE collected this data on the total amount of the Sun’s radiant energy throughout Sept. 2017. The satellite actually detected a dip in total irradiance – or the total amount of energy from the Sun- during the month’s intense solar activity.
But there's still very much we don't know about total solar irradiance. We do not know how it varies over longer timescales. Longer term observations are especially important because scientists have observed unusually quiet magnetic activity from the Sun for the past two decades with previous satellites. During the last prolonged solar minimum in 2008-2009, our Sun was the quietest it has ever been since we started observations in 1978. Scientists expect the Sun to enter a solar minimum within the next three years, and TSIS-1 will be primed to take measurements of the next minimum and see if this is part of a larger trend.
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