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The <strong>Earth</strong> Observer July - August 2012 Volume 24, Issue 4 17<br />

SORCE SSI Workshop Summary<br />

Jerald Harder, Laboratory for Atmospheric and Space Physics, University of Colorado, jerry.harder@lasp.colorado.edu<br />

Joseph Rice, National Institute of Standards and Technology, joe.rice@nist.gov<br />

Martin Snow, Laboratory for Atmospheric and Space Physics, University of Colorado, marty.snow@lasp.colorado.edu<br />

Thomas Woods, Laboratory for Atmospheric and Space Physics, University of Colorado, tom.woods@lasp.colorado.edu<br />

From February 28–March 1, 2012, over 30 scientists<br />

and calibration specialists gathered at the National Institute<br />

of Standards and Technology (NIST) in Gaithersburg,<br />

MD, for the first Solar Spectral Irradiance (SSI)<br />

Variations Workshop. The purpose of the workshop was<br />

to address the interesting and conflicting differences for<br />

the SSI variations reported during the Solar Radiation<br />

and Climate Experiment (SORCE) mission and other<br />

missions. The SORCE Science Team, in collaboration<br />

with NIST and NASA’s Goddard Space Flight Center<br />

(GSFC), met with other SSI instrument teams and calibration<br />

experts to examine these discrepancies by focusing<br />

on issues primarily related to understanding degradation<br />

trends that affect the measurement of solar cycle<br />

variations in irradiance. The agenda included:<br />

• Reviewing various SSI instrument observations, capabilities,<br />

and their estimated irradiance uncertainties;<br />

• discussing how each instrument team analyzed the<br />

spectral data, to separate instrument effects (e.g.<br />

degradation) from intrinsic solar variations;<br />

• discussing the reported SSI differences and refinement<br />

of the uncertainties, to gain a better understanding<br />

of them; and<br />

• planning future methods, to identify the significant<br />

differences (e.g., new studies, new calibrations,<br />

etc.) and refine uncertainties.<br />

Artist’s rendering of SORCE in orbit.<br />

A summary of this workshop, including PDF versions<br />

of many of the presentations, is available at lasp.colorado.<br />

edu/sorce/workshops/index.htm.<br />

Gary Rottman [Laboratory for Atmospheric and Space<br />

Physics, University of Colorado (LASP/CU)—Original<br />

SORCE Principal Investigator] opened the workshop<br />

and discussed the challenges in understanding SSI solar<br />

cycle variability. He cautioned that space is a hostile<br />

environment for optical instruments used to observe<br />

the Sun. The responsivity of all instruments changes<br />

with time and exposure for several reasons, but degradation<br />

presents the greatest obstacle to determining solar<br />

variability.<br />

meeting/workshop summaries<br />

A critical requirement for this workshop was that<br />

participants examine the methods used to perform<br />

long-term instrument degradation corrections. The<br />

techniques used for correcting on-orbit irradiance<br />

vary from instrument to instrument, so analysis of<br />

how these corrections are performed and uncertainty<br />

estimates for those corrections are necessary.<br />

Figure 1. [Top] Solar radiation is absorbed differentially across its spectrum<br />

by the <strong>Earth</strong>’s atmosphere. [Bottom] Solar variability predicted<br />

from models based on total solar irradiance (TSI) and ultraviolet SSI<br />

observations [adapted from Solanki and Unruh, 1998]. Horizontal lines<br />

show limits of detectable variability achievable with current instruments<br />

(dotted) and capabilities required to measure solar variability at<br />

visible wavelengths (dashed). Image credit: Gary Rottman<br />

The importance of this problem is shown in Figure 1.<br />

The top panel shows how the solar spectrum is “filtered”<br />

from the top of the atmosphere to the surface, showing<br />

that solar variability is significant throughout the entire<br />

spectrum. The lower panel portrays one model’s estimate<br />

of the solar variability based on partitioning total<br />

solar irradiance (TSI) measurements in the visible/<br />

infrared (VIS/IR) and applying measured variability in<br />

the 200–400-nm range from the Upper Atmosphere

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