SMOS Mission Extended to 2021!

Category : CATDS, Data, L1, L2, L3, L4, Non classé, Satellite

I am glad to inform you that yesterday the Program Board for Earth Observation (PB-EO) of ESA voted the SMOS mission extension following the ACEO (Advisory Committee for Earth Observation) review report:

« Member states’ delegations were very positive about both the achievements so far as well as the detailed plan being put forward for the extension. « 

CNES (the French Space Agency also funding the mission exploitation), has already granted funding until 2021 (actually 2019 with extension to 2021 pending PB-EO vote which we now have).

So, should everything go nicely with the satellite and platform, we have data guaranteed until  2021!

Congratulations and many thanks to all the actors of this success.

SMOS is now over 9 year old and still going strong by the way!

Yann

Special Issue « New Outstanding Results over Land from the SMOS Mission »

Category : Data

from Amen Al-Yaari and Arnaud Mialon

Call for publications

Dear Colleagues,

Surface soil moisture (the water content in the first centimeters of soil) is an essential climate variable that plays an important role in land–atmosphere interactions. Soil moisture is widely used in improving climate model predictions/projections, weather forecasting, drought monitoring, rainfall estimations, etc.

Monitoring surface soil moisture at a global scale has recently become possible thanks to microwave remote sensing. SMOS (Soil Moisture and Ocean Salinity) was the first dedicated soil moisture mission that has been in orbit for eight years. The SMOS satellite was launched by the European Space Agency (ESA) in 2009, carrying on board a radiometer in the L-band frequency with a native spatial resolution of ~43 km. Since then, soil moisture and vegetation optical depth (VOD) have been retrieved from multi-angular brightness temperature observations relying mainly on a radiative transfer model.

This is a dedicated Special Issue on SMOS. We welcome studies on all subjects that are related to the SMOS satellite and its products.

Potential topics include, but are not limited to, the following:

  • the improvements in the soil moisture/VOD retrieval algorithms;
  • the evaluation/validation of the SMOS soil moisture and VOD products;
  • SMOS synergy with other remote sensing observations or models simulations;
  • SMOS soil moisture/VOD applications for agriculture, hydrology, etc.

Dr. Amen Al-Yaari
Dr. Arnaud Mialon
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All papers will be peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Remote Sensing is an international peer-reviewed open access monthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 1800 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI’s English editing service prior to publication or during author revisions.

http://www.mdpi.com/journal/remotesensing/special_issues/smos_rs

Breaking news –> SMOS new LEVEL 2 SM Version in ready!

Category : L2

Dear All

The long awaited SMOS V650 is now ready for release and thus for you to use!

We (ESA and ESLs) have prepared it  tested it, run the reprocessing from beginning to now, and the operational processor is no ready to produce it giving you access to the whole data set!

The main features of the new versions are described in the release note made available with the new distribution. It capitalises as usual on the progresses made at level 1, but the most salient features are

  • the replacement of ECOCLIMAP by IGBP which enables to have i) an up to date land use map and ii) to be aligned with SMAP and Aquarius,
  • the use of CdF matching in mixed forest nominal pixels and much more accurate and
  • relevant DQX and Chi2
  • Finally the way the current files are updated is also improved.

As  a consequence the new version is « wetter » at high latitudes and around forested areas (with also higher VODs), more retrievals are successful. In terms of metrics with respect to our usual sparse and dense networks, both correlation coefficients and RMSE  are improved but also thereis no bias at all while the SDTE remains the same.

V651-SM

Difference (V650-V620) of averaged soil moisture (4 months per year January; April, July and October) during 7 years.

V650-Tau

Difference (V650-V620) of averaged vegetation opacity (4 months per year January; April, July and October) during 7 years.

Data and documentation available at the usual ESA / Array addresses

Note that the SM NRT are being updated. CATDS L3 will also be updated, but after we have corrected an issue with L3 temporal approach algorithm.

Have fun!

New version of the level 3 product is now available

Category : CATDS, L3

Dear  SMOS L3 user,

Since June 24, 2013 (Day of the Year 175), the new version 2.60 of the level 3 processor has been implemented.

It is an important step as the MIRONOV dielectric model is used instead of the Dobson’s one. For those who are familiar with the level 2 data, it is aligned with the V6.0 level 2 processor.

Be careful as you may observe a change in the derived soil moisture as a consequence. A complete reprocessing will be done later this year to have a homogeneous time series. In the mean time be aware of the discrepancy between the two versions and , keep in mind this comment.

To summarize

*) for the new algorithm use products with  « 260 » in the name (referring to the processor used)

e.g., SM_OPER_MIR_CLF31A_20130624T000000_20130624T235959_260_001_7.tgz

*) All lower versions (typically 2.5, 2.4) use the Dobson’s model and are thus prone to be « dryer »

the L3 team

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