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Johannes Lampel

Physiker

Name	Johannes Lampel
Ort	Henstedt-Ulzburg (Geburtsort) Deutschland
Geschlecht	männlich
Akademischer Grad bzw. Titel	Dr. rer. nat. (Univ. Heidelberg) (2014)
Beruf	Physiker (charakteristischer Beruf)
Datensatztyp	Person
GND-Nummer	1058086871
Datensatz-ID	1058086871
Beteiligt an alle anzeigen New methods for the calibration of optical resonators: integrated calibration by means of optical modulation (ICOM) and narrow-band cavity ring-down (NB-CRD) New methods for the calibration of optical resonators: Integrated Calibration by means of Optical Modulation (ICOM) and Narrow Band Cavity ring-down (NB-CRD) Intercomparison of MAX-DOAS vertical profile retrieval algorithms: studies on field data from the CINDI-2 campaign Intercomparison of MAX-DOAS vertical profile retrieval algorithms: studies on field data from the CINDI-2 campaign Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 Campaign Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 campaign MAX-DOAS measurements of NO 2 , SO 2 , HCHO, and BrO at the Mt. Waliguan WMO GAW global baseline station in the Tibetan Plateau Intercomparison of NO2, O-4, O-3 and HCHO slant column measurements by MAX-DOAS and zenith-sky UV-visible spectrometers during CINDI-2 Intercomparison of NO 2 , O 4 , O 3 and HCHO slant column measurements by MAX-DOAS and zenith-sky UV-Visible spectrometers during the CINDI-2 campaign The ICAD (Iterative Cavity Enhanced DOAS) Method Is a scaling factor required to obtain closure between measured and modelled atmospheric O 4 absorptions? An assessment of uncertainties of measurements and radiative transfer simulations for 2 selected days during the MAD-CAT campaign The ESA GOME-Evolution “Climate” water vapor product: a homogenized time series of H 2 O columns from GOME, SCIAMACHY, and GOME-2 Is a scaling factor required to obtain closure between measured and modelled atmospheric O 4 absorptions? – A case study for two days during the MADCAT campaign BOREAS – a new MAX-DOAS profile retrieval algorithm for aerosols and trace gases BOREAS – a new MAX-DOAS profile retrieval algorithm for aerosols and trace gases Detection of O 4 absorption around 328 and 419 nm in measured atmospheric absorption spectra The tilt-effect in DOAS observations The tilt effect in DOAS observations MAX-DOAS measurements of HONO slant column densities during the MAD-CAT campaign: inter-comparison, sensitivity studies on spectral analysis settings, and error budget Investigating differences in DOAS retrieval codes using MAD-CAT campaign data Parameterizing the instrumental spectral response function and its changes by a super-Gaussian and its derivatives Horizontal and vertical structure of reactive bromine events probed by bromine monoxide MAX-DOAS Validation of OMI, GOME-2A and GOME-2B tropospheric NO 2 , SO 2 and HCHO products using MAX-DOAS observations from 2011 to 2014 in Wuxi, China: investigation of the effects of priori profiles and aerosols on the satellite products Ground-based MAX-DOAS observations of tropospheric aerosols, NO 2 , SO 2 and HCHO in Wuxi, China, from 2011 to 2014 Detection of water vapour absorption around 363 nm in measured atmospheric absorption spectra and its effect on DOAS evaluations Retrieval of absolute SO 2 column amounts from scattered-light spectra: implications for the evaluation of data from automated DOAS networks Biogenic halocarbons from the Peruvian upwelling region as tropospheric halogen source. Measurements of reactive trace gases in the marine boundary layer using novel DOAS methods Measurements of reactive trace gases in the marine boundary layer using novel DOAS methods

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Katalog der Deutschen Nationalbibliothek

Johannes Lampel

New methods for the calibration of optical resonators: integrated calibration by means of optical modulation (ICOM) and narrow-band cavity ring-down (NB-CRD)

New methods for the calibration of optical resonators: Integrated Calibration by means of Optical Modulation (ICOM) and Narrow Band Cavity ring-down (NB-CRD)

Intercomparison of MAX-DOAS vertical profile retrieval algorithms: studies on field data from the CINDI-2 campaign

Intercomparison of MAX-DOAS vertical profile retrieval algorithms: studies on field data from the CINDI-2 campaign

Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 Campaign

Inter-comparison of MAX-DOAS measurements of tropospheric HONO slant column densities and vertical profiles during the CINDI-2 campaign

MAX-DOAS measurements of NO 2 , SO 2 , HCHO, and BrO at the Mt. Waliguan WMO GAW global baseline station in the Tibetan Plateau

Intercomparison of NO2, O-4, O-3 and HCHO slant column measurements by MAX-DOAS and zenith-sky UV-visible spectrometers during CINDI-2

Intercomparison of NO 2 , O 4 , O 3 and HCHO slant column measurements by MAX-DOAS and zenith-sky UV-Visible spectrometers during the CINDI-2 campaign

The ICAD (Iterative Cavity Enhanced DOAS) Method

Is a scaling factor required to obtain closure between measured and modelled atmospheric O 4 absorptions? An assessment of uncertainties of measurements and radiative transfer simulations for 2 selected days during the MAD-CAT campaign

The ESA GOME-Evolution “Climate” water vapor product: a homogenized time series of H 2 O columns from GOME, SCIAMACHY, and GOME-2

Is a scaling factor required to obtain closure between measured and modelled atmospheric O 4 absorptions? &ndash; A case study for two days during the MADCAT campaign

BOREAS &ndash; a new MAX-DOAS profile retrieval algorithm for aerosols and trace gases

BOREAS – a new MAX-DOAS profile retrieval algorithm for aerosols and trace gases

Detection of O 4 absorption around 328 and 419 nm in measured atmospheric absorption spectra

The tilt-effect in DOAS observations

The tilt effect in DOAS observations

MAX-DOAS measurements of HONO slant column densities during the MAD-CAT campaign: inter-comparison, sensitivity studies on spectral analysis settings, and error budget

Investigating differences in DOAS retrieval codes using MAD-CAT campaign data

Parameterizing the instrumental spectral response function and its changes by a super-Gaussian and its derivatives

Horizontal and vertical structure of reactive bromine events probed by bromine monoxide MAX-DOAS

Validation of OMI, GOME-2A and GOME-2B tropospheric NO 2 , SO 2 and HCHO products using MAX-DOAS observations from 2011 to 2014 in Wuxi, China: investigation of the effects of priori profiles and aerosols on the satellite products

Ground-based MAX-DOAS observations of tropospheric aerosols, NO 2 , SO 2 and HCHO in Wuxi, China, from 2011 to 2014

Detection of water vapour absorption around 363 nm in measured atmospheric absorption spectra and its effect on DOAS evaluations

Retrieval of absolute SO 2 column amounts from scattered-light spectra: implications for the evaluation of data from automated DOAS networks

Biogenic halocarbons from the Peruvian upwelling region as tropospheric halogen source.

Measurements of reactive trace gases in the marine boundary layer using novel DOAS methods

Measurements of reactive trace gases in the marine boundary layer using novel DOAS methods

Is a scaling factor required to obtain closure between measured and modelled atmospheric O 4 absorptions? – A case study for two days during the MADCAT campaign

BOREAS – a new MAX-DOAS profile retrieval algorithm for aerosols and trace gases

Detection of O 4 absorption around 328 and 419 nm in measured atmospheric absorption spectra

Detection of water vapour absorption around 363 nm in measured atmospheric absorption spectra and its effect on DOAS evaluations