4.2. Radiation environment

The L2 environment (and orbits around it) is relatively benign compared to those in geostationary (GO), or low Earth (LEO) orbits. In particular, a series of common threats for satellites in GO or LEO, including the neutral thermosphere, space debris, geomagnetically trapped particles and large temperature gradients, are not a concern for L2 orbits. Environmental aspects to be considered at L2 include:

Therefore, the main radiation components at L2 consist of: Galactic cosmic rays, solar particle events and solar and Jovian electrons. Solar activity follows an 11-year cycle. The last minimum occurred in December 2008 and therefore the Herschel launch in 2009 was carried out during a low activity state. Contrary to former predictions, the next solar cycle will be below average in intensity, with a predicted maximum sunspot number of 90. Given the predicted date of solar minimum and the predicted maximum intensity, solar maximum is now expected to occur in May, 2013 (Solar Cycle 24 Prediction Panel agreement on May 8, 2009). Therefore Solar particle events are expected to be problematic only towards the end of the mission. At the time of writing the AO-2 version of this manual (March 2011), the solar activity is increasing, the proton event observed in OD 663 (7-8 March 2011) being the strongest one observed to date. Notably, there is no noticeable impact of this increased solar activity in the performance of the instruments or the quality of the science products at the levels of activity observed so far (maximum ~50 proton flux units in the March 7/8 event).

Weekly, calibrated plots of the Herschel SREM data and special plots of any observed proton events are available to users, provided by the SREM PI, Petteri Nieminen. These are available at http://proteus.space.noa.gr/~srem/herschel/.

In the early stages of the mission, the dominant radiation source has been Jovian electrons, characterised by a energetic population and a 13-month synodic year modulation. Solar electrons will be an important source at lower energies with abrupt peak emissions, and a 27-day period.

The Herschel spacecraft is equipped with a standard radiation environment monitor (SREM) placed in the -Z SVM panel; the SREM is a particle detector developed for satellite applications that has been added to Herschel and Planck as a passenger. It measures high-energy electrons (from 0.5 MeV to infinity) and protons (from 20 MeV to infinity) of the space environment with an angular resolution of some 20 degrees, providing particle species and spectral information. The SREM data are received on-ground and processed by the Space Weather Group at ESTEC, providing valuable information on the radiation environment at L2. A sample plot showing the calibrated count rates in three counters (TC1 - protons with E > 20 MeV; TC2 - protons with E > 39 MeV; TC3 - electrons with E > 0.5 MeV) is displayed in Figure 4.3 .

SREM calibrated count rates in three counters (TC1, TC2 and TC3), rebinned in intervals of five minutes. from the 30th of October 2009 (OD 170) to 27th March of 2011 (OD 683). The slight decline of the count rates can be explained by an increased solar activity and the subsequent increase of shielding to Galactic cosmic rays. Several events are visble, the most conspicuous a proton flare detected in OD 663 (7-8 March 2011).

Figure 4.3.  SREM calibrated count rates in three counters (TC1, TC2 and TC3), rebinned in intervals of five minutes. from the 30th of October 2009 (OD 170) to 27th March of 2011 (OD 683). The slight decline of the count rates can be explained by an increased solar activity and the subsequent increase of shielding to Galactic cosmic rays. Several events are visble, the most conspicuous a proton flare detected in OD 663 (7-8 March 2011).