By Tushna Commissariat

Astronomy and astrophysics has has advanced in leaps and bounds over the past few decades. As mankind attempts to foray further into the universe, it’s the little things that get by us sometimes.

Star formation is an area that has been well researched and studied and though we understand the ‘how’ and the ‘why’ of stellar genesis and evolution; it is very difficult to get visual evidence for theoretical data.

Images of Orion Nebula - a star forming area - taken by Plank... Image credit: ESA, LFI and HFI Consortia

In our home galaxy, the Milky Way, there are an expected 100-400 billion stars. But weaving through this mass of stars are vast clouds of gas and dust that are generally referred to as the interstellar medium (ISM).

Now as much as the ISM might sound like a really cool name for dirt in space right out of Star Trek, it’s this very dust that obscures our views of new-born stars in visible light.

If we tune our instruments to look with longer wavelengths, especially where the Cosmic Microwave Background can be penetrated, lo and behold, a much clearer picture awaits us!

The dust no longer blocks the emission from the innermost regions of the galaxy and details previously unseen are revealed. New images from ESA ‘s Planck mission have revealed precisely this, isolating actual physical processes at work.

... and by Digitised Sky Survey of the same area in visible wavelength. Image credit: STScI DSS

How does Planck mapping work?

Planck maps the sky in nine frequencies using two state-of-the-art instruments, designed to produce high-sensitivity, multi-frequency measurements of the diffuse sky radiation: the High Frequency Instrument (HFI) includes the frequency bands 100 – 857 GHz, and the Low Frequency Instrument (LFI) includes the frequency bands 30-70 GHz.

The first Planck all-sky survey began in August 2009 and will be completed by late-May 2010. Planck will gather data until the end of 2012, by which time it should complete four sky scans.

At the lowest frequencies, Planck notes emissions that occur due to relativistic electrons moving at relativistic speeds that interact with the Galactic magnetic fields (also known as synchrotron emissions), and that of free-free emission arising from electrons interacting with hot gas (they are called ‘free-free’ emissions as the electrons remain free even after they cause emission of a photon.).

At intermediate frequencies (corresponding to wavelengths of a few millimetres), the emission are mainly thermal emission of ionised gas heated by newly-formed hot stars.

At the highest frequencies, Planck maps the distribution of interstellar dust, including the coldest compact cores in the final stages of collapse towards the formation of new stars.

A star is made

Once stars are formed, they disperse the surrounding molecular clouds. An equilibrium between cloud collapse and dispersion regulates the number of stars that any given galaxy makes.

Various other physical phenomena influence this balance, including gravity, heating and cooling, turbulence, magnetic fields and more.

As a result of this interplay, the ISM rearranges itself into ‘phases’ which coexist side-by-side; so the molecular clouds that contain dense and cool gas and dust and the ‘cirrus’ containing more diffuse and warmer material.

The only way to accurately have data on the phases and constitutional elements of the ISM is to look at it through multiple frequencies; something that Plank can do.

As Plank can study all the mechanisms simultaneously, we can get data of all processes at the same time which is very beneficial. Also as it maps different areas; we can compare the difference seen in the ISM in a star forming area, such as the Orion Nebula with that seen in a low star formation area.

Recent images from Plank have shown us just that. For more information on the planck mission as we as star formation please visit the ESA Planck homepage.

By Nan King

Passing through atmospheres, whether it be earth, mars or titan, poses problems in space exploration. Nan visited The Von Karman Institute in Brussels where research is going on into some unlikely new material that could be used to insulate space craft.

Nan’s trip to Von Karman was thanks to the EU funded project RELATE which has sent 80 science journalists to report on all kinds of research going on at centres across Europe. To find out more about the success of this valuable project visit http://relateproject.eu/

By Tiffany Stecker

The launch of CryoSat-2 , the first ever satellite designed to measure the thickness of polar ice sheets, did not happen.

This news comes as a particular disappointment. The European Space Agency (ESA) -backed mission follows a failed attempt to launch the original CryoSat mission in 2005.

Photo credit: ESA/W. Simpson

But just six days before the 25 February launch date, the reins were pulled once again. Technicians from Yuzhnoye, the manufacturer of CryoSat-2, decided that the fuel tank capacity and fuel gauge margins were not optimal for launching the satellite 700km into space.

“You know when you’re driving, and the fuel gauge shows that you are running out, but there is still enough fuel left, you’re touching in the red zone?” asked Dr Richard Francis, project manager for the mission. In this case, the crew deemed that fuel margin, or “red zone”, too narrow.

To create a larger margin, technicians will change the fuel mixture to a leaner formula to run more efficiently, said Dr Francis.

“The satellite is still safe, this is the important factor,” he said.

CryoSat-2 is designed to emit radar beams that ricochet off the surface of the ice, as well as ocean water surface. The difference in echo between the two is used to assess the thickness of the ice. While the ESA has mapped the extent of ice sheets for more than 15 years, the thickness of ice has never been mapped from space. Data on thickness would further understanding of changes in ice structure in relation to climate change.

On site in Baikonur, Kazakhstan, and at the ESA’s European Spacecraft Operations Centre in Darmstadt, Germany, the mood was somber.

“As you can imagine, the news went down like a lead balloon here,” stated CryoSat campaign manager Bill Simpson on the ESA’s online launch diary.

The ESA hopes to finally launch the satellite four weeks from the original launch date, although no official announcement has been made. A team of experts will meet this week in Ukraine, where Yuzhnoye is based, to discuss the course of action to repair the satellite.

The 2005 failure was caused by a missing command from the onboard flight control system. When the main engine cut-off was to occur, the command was lost as the engine continued to operate until it ran out of fuel. Thus, the two parts of the satellite did not separate as planned, and the entire satellite crashed close to the North Pole.

More than four years later, the project has bloated to approximately €250m (£220m), according to Dr Duncan Wingham, lead investigator for the mission and professor of climate physics at University College London.

Yuzhnoye is unable to give a figure on the cost of reformulating CryoSat-2 before the next planned launch, said Oleg Ventskovsky, a representative from the company’s Brussels, Belgium office. He assured that the company would absorb all costs incurred. ESA is funded by European Union member states who contribute a percentage of their Gross Domestic Product (GDP) to the agency.

CryoSat was the first mission in the ESA’s Earth Explorers programme to be selected in 1999. Two other satellites have already been launched as part of the programme: the Gravity field and steady-state Ocean Circulation Explorer (GOCE) mission [ GOCE] to improve models of the Earth’s gravity fields was launched on 17 March last year, and the Soil Moisture and Ocean Salinity (SMOS) mission to measure moisture and salinity levels was launched on 2 November.

“Those of us who went through the failure the first time around are feeling a little bit nervous this time,” said Dr Wingham in an interview before the delay. “But I do hope that we don’t have to wait another five years to get this mission into space.”

By Jenn Green

The chance of detecting extra terrestrial life is now greater than ever before, Lord Martin Rees told scientists two weeks ago at a Royal Society conference in London. The meeting discussed current developments in the search for alien life and its consequences for science and society.

Lord Rees, President of the society, claims that with new technology it will now be possible to detect earth-like planets orbiting other stars, focusing the search for extra terrestrials.

“Were we to find life, even the simplest life, elsewhere that would clearly be one of the great discoveries of the 21st Century”, he said.

He told the audience that if life was discovered in outer space he suspected it would be in intelligent forms that we would not be able to conceive.

“There could be forms of intelligence beyond human capacity, beyond as much as we are beyond a chimpanzee”, he said.

However Dr Lewis Dartnell, astrobiologist and author of the book ‘Life in the Universe’, thought that the difference between humans and aliens could be starker than this, as intelligent life would have evolved somewhere in the galaxy over the last four or five billion years.

“It would not even be the comparison between chimpanzees and humans, it would be between humans and something we possibly could not even conceive, and maybe will not even be able to recognise.”

“If we come across an intelligent species they would appear like Gods to us,” explains Dartnell. “They would have such advanced technology we would not be able to distinguish it from magic.”