GeminiFocus 2018 Year in Review | Page 66

Figure 13. A small section of the IGRINS first-light spectrum. Purple - IGRINS spectrum of TW Hya from Gemini South. A small part of the K band in both cases. Green - combination of multiple epochs of spectra on the same object from McDonald Observatory [Figure from Sokal et al., 2018] Figure 14. IGRINS first-block (April) observing statistics. but it produced a spectrum that rivals the hard-earned published one from McDon- ald Observatory (Figure 13). With such remarkable first impressions, the IGRINS team is extremely excited to be sharing the IGRINS+Gemini combination with Gemini’s broad astronomical community, and as its 2018 observing blocks at Gemini South draw to a close, we all look forward to the exciting results to come. IGRINS was scheduled for three separate observing blocks in Semester 2018A. As this issued goes to e-press IGRINS’ time at Gemini South is complete for now. In the first block, apart from worse than usual weather and one significant fault due to a compressor failure (Figure 14), we’ve spent almost the entire time observing IGRINS programs with one or two observations done in the regular queue. Hopefully the weather will hold up through the second and third blocks, but it’s already apparent that IGRINS is a very powerful (as well as popular) visitor instrument to Gemini. Daniel Jaffe of UT Austin is the IGRINS Prin- cipal Investigator (PI). Chan Park of KASI is deputy PI and KASI instrument PI. Jae-Joon Lee at KASI supervises the IGRINS operation- al program on the Korean side. The IGRINS visit to Gemini is supported by the U.S. National Science Foundation under grant AST-1702267 (PI - Gregory Mace, University of Texas at Austin), and by the Korean GMT Project of KASI. Further technical details are available in Yuk, et al. (2010) (view here), and Mace, et al. (2016) (view here). IGRINS sci- ence support at Gemini is provided by Hwi- hyun Kim. Volcano Watch Activity at Gemini North Hawai‘i Island has suffered a long series of major earthquakes and lava eruptions in the “East Rift” zone of the Kilauea volca- no, and a large number of smaller quakes and ash emissions from the summit crater, Halema‘uma‘u. While all of this action is a 60-mile drive or more from Maunakea, it 64 GeminiFocus January 2019 / 2018 Year in Review