Abstract. Carbon dioxide (CO 2 ) and Methane (CH 4 ) are the two most important anthropogenic greenhouse gases. CH 4 is furthermore one of the most potent present and future contributors to global warming because of its large global warming potential (GWP). Our knowledge of CH 4 and CO 2 source strengths is based primarily on bottom-up scaling of sparse in-situ local point measurements of emissions and upscaling of emission factor estimates or top-down modeling incorporating data from surface networks and more recently also by incorporating data from low spatial resolution satellite observations for CH 4 . There is a need to measure and retrieve the dry columns of CO 2 and CH 4 having high spatial resolution and spatial coverage. In order to fill this gap a new passive airborne 2-channel grating spectrometer instrument for remote sensing of small scale and mesoscale column-averaged CH 4 and CO 2 observations has been developed. This Methane Airborne MAPper (MAMAP) instrument measures reflected and scattered solar radiation in the short wave infrared (SWIR) and near-infrared (NIR) parts of the electro-magnetic spectrum at moderate spectral resolution. The SWIR channel yields measurements of atmospheric absorption bands of CH 4 and CO 2 in the spectral range between 1.59 and 1.69 µm at a spectral resolution of 0.82 nm. The NIR channel around 0.76 µm measures the atmospheric O 2 -A-band absorption with a resolution of 0.46 nm. MAMAP has been designed for flexible operation aboard a variety of airborne platforms. The instrument Correspondence to: K. Gerilowski (gerilows@iup.physik.uni-bremen.de) design and the performance of the SWIR channel, together with some results from on-ground and in-flight engineering tests are presented. The SWIR channel performance has been analyzed using a retrieval algorithm applied to the nadir measured spectra. Dry air column-averaged mole fractions are obtained from SWIR data only by dividing the retrieved CH 4 columns by the simultaneously retrieved CO 2 columns for dry air column CH 4 (XCH 4 ) and vice versa for dry air column CO 2 (XCO 2 ). The signal-to-noise ratio (SNR) of the SWIR channel is approximately 1000 for integration times (t int ) in the range of 0.6-0.8 s for scenes with surface spectral reflectances (SSR)/albedo of around 0.18. At these integration times the ground scene size is about 23 ×33 m 2 for an aircraft altitude of 1 km and a ground speed of 200 km/h. For these scenes the actual XCH 4 or XCO 2 dry air column retrieval precisions are typically about 1% (1 σ ). Elevated levels of CH 4 have been retrieved above a CH 4 emitting landfill. Similarly the plume of CO 2 from coal-fired power plants can be well detected and tracked. The measurements by the MAMAP sensor could enable estimates of anthropogenic, biogenic and geological emissions of localized intense CH 4 and CO 2 sources such as anthropogenic fugitive CH 4 emissions from oil and gas industry, coal mining, disposal of organic waste, CO 2 emissions from coal-fired power plants, steel production or geologic ...

The water Vapour Emission SPectrometer for Antarctica at 22 GHz (VESPA-22) has been designed for long-term middle atmospheric climate change monitoring and satellite data validation. It observes the water vapour spectral line at 22.235 GHz using the balanced beam-switching technique. The receiver antenna has been characterized, showing an HPBW of 3.5° and a sidelobe level 40 dB below the main lobe. The receiver front-end has a total gain of 105 dB and a LNA noise temperature of 125 K. A FFT spectrometer (bandwidth 1 GHz, resolution 63 kHz) will be used as back-end, allowing the retrieval of H 2 O concentration profiles in the 20 to 80 km altitude range. The control I/O interface is based on reconfigurable hardware (USB-CPLD).

Carbon dioxide (CO₂) and Methane (CH₄) are the two most important anthropogenic greenhouse gases. CH₄ is furthermore one of the most potent present and future contributors to global warming because of its large global warming potential (GWP). Our knowledge of CH₄ sources and sinks is based primarily on sparse in-situ local point measurements from micro sites and surface networks and more recently on low spatial resolution satellite observations. There is a need for measurements of the dry columns of CO₂ and CH₄ having high spatial resolution and spatial coverage. In order to fill this gap a new passive airborne 2-channel grating spectrometer instrument for remote sensing of small scale and mesoscale column-averaged CH₄ and CO₂ observations has been developed. This Methane Airborne MAPper (MAMAP) instrument measures reflected and scattered solar radiation in the short wave infrared (SWIR) and near-infrared (NIR) parts of the electro-magnetic spectrum at moderate spectral resolution. The SWIR channel yields measurements of atmospheric absorption bands of CH₄ and CO₂ in the spectral range between 1.59 and 1.69 μm at a spectral resolution of 0.82 nm. The NIR channel around 0.76 μm measures the atmospheric O₂-A-band absorption with a resolution of 0.46 nm. MAMAP has been designed for flexible operation aboard a variety of airborne platforms. The instrument design and performance, together with some results from on-ground and in-flight engineering tests are presented. The instrument performance has been analyzed using a retrieval algorithm applied to the SWIR channel nadir measured spectra. The signal-to-noise ratio (SNR) of the SWIR channel is approximately 1000 for integration times (t_int) in the range of 0.6–0.8 s for scenes with surface spectral reflectances of around 0.18. At these integration times the ground scene size is about 23×33 m² for an aircraft altitude of 1 km and a ground speed of 200 km/h. For these scenes the CH₄ and CO₂ column retrieval precisions are typically about 1% (1 σ). Elevated levels of CH₄ have been retrieved above a CH₄ emitting landfill. Similarly the plume of CO₂ from coal-fired power plants can be well detected and tracked. The measurements by the MAMAP sensor enable estimates of anthropogenic, biogenic and geological emissions of localized intense CH₄ and CO₂ sources such as anthropogenic fugitive emissions from gas industry and waste, emissions from coal-fired power plants or geologic emissions from seepage and volcanoes. Appropriate analysis of the measurements of MAMAP potentially also yields CH₄ emissions from less intense but extensive sources such as wetlands