000902606 001__ 902606
000902606 005__ 20240712100905.0
000902606 0247_ $$2doi$$a10.1515/teme-2021-0043
000902606 0247_ $$2ISSN$$a0170-575X
000902606 0247_ $$2ISSN$$a0171-8096
000902606 0247_ $$2ISSN$$a0340-4021
000902606 0247_ $$2ISSN$$a0340-837X
000902606 0247_ $$2ISSN$$a0365-7418
000902606 0247_ $$2ISSN$$a2196-7113
000902606 0247_ $$2Handle$$a2128/29213
000902606 0247_ $$2WOS$$aWOS:000696298100009
000902606 037__ $$aFZJ-2021-04401
000902606 082__ $$a620
000902606 1001_ $$0P:(DE-HGF)0$$aStehr, Johannes$$b0$$eCorresponding author
000902606 245__ $$aGRIPS-HI, a novel spectral imager for ground based measurements of mesopause temperatures
000902606 260__ $$aBerlin$$b˜Deœ Gruyter$$c2021
000902606 3367_ $$2DRIVER$$aarticle
000902606 3367_ $$2DataCite$$aOutput Types/Journal article
000902606 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1638254397_15499
000902606 3367_ $$2BibTeX$$aARTICLE
000902606 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000902606 3367_ $$00$$2EndNote$$aJournal Article
000902606 520__ $$aThe NDMC (Network for the Detection of Mesospheric Change) is a global network of measurement sites dedicated to the surveillance of the mesopause region. One main objective of the network is the early identification of climate signals. A key parameter is the mesopause temperature which can be derived from the emission spectrum of a layer of vibrationally excited hydroxyl (OH) at an altitude of approximately 87km. Foremost, emission lines in the SWIR regime between 1520nm and 1550nm are of interest for remote temperature sensing. This report deals with the development of a new generation of GRIPS instruments, which are commonly employed for the observation of mesopause temperatures. The new prototype demonstrates how the application of so called Spatial Heterodyne Interferometers (SHI) can overcome the limitations of currently used grating spectrometers, in terms of spectral resolution and optical throughput. The presented prototype proposes improvements in optical throughput and spectral resolution of about one order of magnitude, significantly reducing the uncertainties of the measured mesopause temperatures. Furthermore, an SHI can be built in monolithic configurations which are aligned and characterized once during assembly without the need of realignment at the measurement site. This makes SHI based instruments ideal for mobile applications.
000902606 536__ $$0G:(DE-HGF)POF4-2112$$a2112 - Climate Feedbacks (POF4-211)$$cPOF4-211$$fPOF IV$$x0
000902606 588__ $$aDataset connected to CrossRef, Journals: juser.fz-juelich.de
000902606 7001_ $$0P:(DE-HGF)0$$aKnieling, Peter$$b1
000902606 7001_ $$0P:(DE-Juel1)177834$$aOlschewski, Friedhelm$$b2$$ufzj
000902606 7001_ $$0P:(DE-HGF)0$$aMantel, Klaus$$b3
000902606 7001_ $$0P:(DE-Juel1)129128$$aKaufmann, Martin$$b4$$ufzj
000902606 7001_ $$0P:(DE-Juel1)16343$$aKoppmann, Ralf$$b5
000902606 773__ $$0PERI:(DE-600)2025790-9$$a10.1515/teme-2021-0043$$gVol. 88, no. 10, p. 655 - 660$$n10$$p655 - 660$$tTechnisches Messen$$v88$$x0170-575X$$y2021
000902606 8564_ $$uhttps://juser.fz-juelich.de/record/902606/files/TEME-2021-0043_v1.1_Korrektur.pdf$$yOpenAccess
000902606 909CO $$ooai:juser.fz-juelich.de:902606$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000902606 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)177834$$aForschungszentrum Jülich$$b2$$kFZJ
000902606 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)129128$$aForschungszentrum Jülich$$b4$$kFZJ
000902606 9131_ $$0G:(DE-HGF)POF4-211$$1G:(DE-HGF)POF4-210$$2G:(DE-HGF)POF4-200$$3G:(DE-HGF)POF4$$4G:(DE-HGF)POF$$9G:(DE-HGF)POF4-2112$$aDE-HGF$$bForschungsbereich Erde und Umwelt$$lErde im Wandel – Unsere Zukunft nachhaltig gestalten$$vDie Atmosphäre im globalen Wandel$$x0
000902606 9141_ $$y2021
000902606 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)1160$$2StatID$$aDBCoverage$$bCurrent Contents - Engineering, Computing and Technology$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bTM-TECH MESS : 2019$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000902606 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2021-01-27
000902606 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2021-01-27
000902606 920__ $$lyes
000902606 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$kIEK-7$$lStratosphäre$$x0
000902606 9801_ $$aFullTexts
000902606 980__ $$ajournal
000902606 980__ $$aVDB
000902606 980__ $$aUNRESTRICTED
000902606 980__ $$aI:(DE-Juel1)IEK-7-20101013
000902606 981__ $$aI:(DE-Juel1)ICE-4-20101013