Evelyn Jäkel

ORCID: 0009-0008-9181-3432
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About
Contact & Profiles
Research Areas
  • Atmospheric aerosols and clouds
  • Atmospheric chemistry and aerosols
  • Arctic and Antarctic ice dynamics
  • Atmospheric and Environmental Gas Dynamics
  • Atmospheric Ozone and Climate
  • Cryospheric studies and observations
  • Calibration and Measurement Techniques
  • Infrared Target Detection Methodologies
  • Climate change and permafrost
  • Remote Sensing in Agriculture
  • Meteorological Phenomena and Simulations
  • Aeolian processes and effects
  • Spacecraft Design and Technology
  • Solar Radiation and Photovoltaics
  • Spacecraft and Cryogenic Technologies
  • Radiative Heat Transfer Studies
  • Polar Research and Ecology
  • Impact of Light on Environment and Health
  • Climate variability and models
  • Methane Hydrates and Related Phenomena
  • Ionosphere and magnetosphere dynamics
  • Air Quality and Health Impacts
  • Spacecraft Dynamics and Control
  • Geochemistry and Geologic Mapping
  • Urban Heat Island Mitigation

Leipzig University
2015-2024

Max Planck Institute for Meteorology
2013

Johannes Gutenberg University Mainz
2008-2010

Leibniz Institute for Tropospheric Research
2004-2008

National Institute for Public Health and the Environment
2007

German Meteorological Service
2007

Leibniz Association
2006

European Space Research and Technology Centre
1980-1998

Wissenschaftliches Institut der AOK
1990

Abstract Clouds play an important role in Arctic amplification. This term represents the recently observed enhanced warming of relative to global increase near-surface air temperature. However, there are still knowledge gaps regarding interplay between clouds and aerosol particles, surface properties, as well turbulent radiative fluxes that inhibit accurate model simulations climate system. In attempt resolve this so-called cloud puzzle, two comprehensive closely coordinated field studies...

10.1175/bams-d-18-0072.1 article EN cc-by Bulletin of the American Meteorological Society 2018-11-07

Abstract Between 1 September and 4 October 2014, a combined airborne ground-based measurement campaign was conducted to study tropical deep convective clouds over the Brazilian Amazon rain forest. The new German research aircraft, High Altitude Long Range Research Aircraft (HALO), modified Gulfstream G550, extensive instrumentation were deployed in near Manaus (State of Amazonas). part German–Brazilian Aerosol, Cloud, Precipitation, Radiation Interactions Dynamics Convective Cloud...

10.1175/bams-d-14-00255.1 article EN other-oa Bulletin of the American Meteorological Society 2016-01-28

Abstract Ice nucleating particles (INPs) affect the radiative properties of cold clouds. Knowledge concerning their concentration above ground level and potential sources is scarce. Here we present first highly temperature resolved ice nucleation spectra airborne samples from an aircraft campaign during late winter in 2018. Most INP featured low levels (<3 · 10 −4 L −1 at −15°C). However, also found concentrations up to 1.8·10 −2 −15°C freezing onsets as high −7.5°C for mainly marine...

10.1029/2020gl087770 article EN Geophysical Research Letters 2020-06-10

Abstract A configuration of the High-Altitude Long-Range Research Aircraft (HALO) as a remote sensing cloud observatory is described, and its use illustrated with results from first second Next-Generation Remote Sensing for Validation (NARVAL) field studies. Measurements NARVAL (NARVAL2) are used to highlight ability HALO, when configured in this fashion, characterize not only distribution water condensate atmosphere, but also impact on radiant energy transfer covarying large-scale...

10.1175/bams-d-18-0198.1 article EN Bulletin of the American Meteorological Society 2019-01-18

Abstract. The concept of cloud radiative forcing (CRF) is commonly applied to quantify the impact clouds on surface energy budget (REB). In Arctic, specific interactions between microphysical and macrophysical properties strongly modify warming or cooling effect clouds, complicating estimate CRF obtained from observations models. Clouds tend increase broadband albedo over snow sea ice surfaces compared cloud-free conditions. However, this not adequately considered in derivation Arctic so...

10.5194/acp-20-9895-2020 article EN cc-by Atmospheric chemistry and physics 2020-08-26

Abstract Melt ponds forming on Arctic sea ice in summer significantly reduce the surface albedo and impact heat mass balance of ice. Therefore, their areal coverage, which can undergo rapid change, is crucial to monitor. We present a revised method extract melt pond fraction (MPF) from Sentinel‐2 satellite imagery, evaluated by MPF products higher‐resolution helicopter‐borne imagery. The analysis evolution during MOSAiC campaign 2020, shows split Central Observatory (CO) into level highly...

10.1029/2022gl102102 article EN cc-by Geophysical Research Letters 2023-03-04

Surface reflectance (SR) estimation is the most critical preprocessing step for deriving geophysical parameters in multi-sensor remote sensing. Most state-of-the-art SR methods, such as vector version of Second Simulation Satellite Signal Solar Spectrum (6SV) radiative transfer (RT) model, depend on accurate information aerosol and atmospheric gases. In this study, a Simplified Robust Reflectance Estimation Method (SREM) based equations from 6SV RT without integrating particles gasses,...

10.3390/rs11111344 article EN cc-by Remote Sensing 2019-06-04

Abstract. Vertical profiles of the cloud particle phase state in tropical deep-convective clouds (DCCs) were investigated using airborne solar radiation data collected by German research aircraft HALO during ACRIDICON-CHUVA campaign, which was conducted over Brazilian Amazon September 2014. A discrimination retrieval based on imaging spec-troradiometer measurements side spectral reflectivity applied to DCCs under different aerosol conditions. From results height mixed layer determined. The...

10.5194/acp-2017-64 article EN cc-by 2017-02-01

Abstract. The Arctic CLoud Observations Using airborne measurements during polar Day (ACLOUD) campaign was carried out north-west of Svalbard (Norway) between 23 May and 6 June 2017. objective ACLOUD to study boundary layer mid-level clouds their role in amplification. Two research aircraft (Polar 5 6) jointly performed 22 flights over the transition zone open ocean closed sea ice. Both were equipped with identical instrumentation for basic meteorological parameters, as well turbulent...

10.5194/essd-11-1853-2019 article EN cc-by Earth system science data 2019-11-29

Abstract. Global warming is amplified in the Arctic. However, numerical models struggle to represent key processes that determine Arctic weather and climate. To collect data help constrain models, HALO–(𝒜𝒞)3 aircraft campaign was conducted over Norwegian Greenland seas, Fram Strait, central Ocean March April 2022. The focused on one specific challenge posed by namely reasonable representation of transformations air masses during their meridional transport into out via northward moist-...

10.5194/acp-24-8865-2024 article EN cc-by Atmospheric chemistry and physics 2024-08-13

Airborne measurements of the ratio spectral upward and downward irradiances (so‐called albedo) are used to derive areal surface albedo in wavelength range from 330 1670 nm. The data were collected over different sea land surfaces cloudless atmospheric conditions during three field campaigns. Measurements Albedometer (developed at IfT) NASA Solar Spectral Flux Radiometer (SSFR) employed. radiative transfer calculations show that scattering absorption within layer beneath flight level...

10.1029/2003jd004392 article EN Journal of Geophysical Research Atmospheres 2004-04-16

Two airborne field campaigns focusing on observations of Arctic mixed-phase clouds and boundary layer processes their role with respect to amplification have been carried out in spring 2019 late summer 2020 over the Fram Strait northwest Svalbard. The latter campaign was closely connected Multidisciplinary drifting Observatory for Study Climate (MOSAiC) expedition. Comprehensive datasets cloudy atmosphere collected by operating remote sensing instruments, in-situ probes, instruments...

10.1038/s41597-022-01900-7 article EN cc-by Scientific Data 2022-12-29

Abstract. The global warming is amplified in the Arctic. To collect data that help to constrain weather and climate models, which often do not realistically represent enhanced Arctic warming, HALO-(AC)³ aircraft campaign was conducted March April 2022 over Norwegian Greenland Seas, Fram Strait, central Ocean. Observations were made areas of open ocean, marginal sea ice zone, ice. Two low-flying one long-range, high-altitude research have been employed. Whenever possible, three flown...

10.5194/egusphere-2024-783 preprint EN cc-by 2024-03-26

Abstract. The combination of downward-looking airborne lidar, radar, microwave, and imaging spectrometer measurements was exploited to characterize the vertical small-scale (down 10 m) horizontal distribution thermodynamic phase low-level Arctic mixed-layer clouds. Two cloud cases observed in a cold air outbreak warm advection event during CLoud Observations Using polar Day (ACLOUD) campaign were investigated. Both exhibited typical mixed-phase structure with mostly liquid water droplets at...

10.5194/acp-20-5487-2020 article EN cc-by Atmospheric chemistry and physics 2020-05-12

Abstract. Low-level airborne observations of the Arctic surface radiative energy budget are discussed. We focus on terrestrial part budget, quantified by thermal-infrared net irradiance (TNI). The data were collected in cloudy and cloud-free conditions over vicinity marginal sea ice zone (MIZ) close to Svalbard during two aircraft campaigns conducted spring 2019 early summer 2017. measurements, complemented ground-based available from literature transfer simulations, used evaluate influence...

10.5194/acp-23-9647-2023 article EN cc-by Atmospheric chemistry and physics 2023-08-31

The reflection, absorption, and transmittance of shortwave solar radiation by sea ice play crucial roles in physical biological processes the ice-covered Arctic Ocean atmosphere. These sea-ice optical properties, particularly during melt season, significantly impact energy fluxes within total budget coupled atmosphere-ice-ocean system. We analyzed data from autonomous drifting stations to investigate seasonal evolution spectral albedo, transmittance, absorptivity for different sea-ice, snow,...

10.1525/elementa.2023.00130 article EN cc-by Elementa Science of the Anthropocene 2024-01-01

Abstract. The sensitivity of passive remote sensing measurements to retrieve microphysical parameters convective clouds, in particular their thermodynamic phase, is investigated by three-dimensional (3-D) radiative transfer simulations. effects different viewing geometries and vertical distributions the cloud properties are investigated. Measurement examples spectral solar radiance reflected sides (passive) near-infrared (NIR) range performed together with collocated lidar observations...

10.5194/amt-6-539-2013 article EN cc-by Atmospheric measurement techniques 2013-03-01

Abstract. For large-scale and long-term Arctic climate simulations appropriate parameterization of the surface albedo is required. Therefore, sea ice (SIS) coupled regional model HIRHAM–NAOSIM was examined against broadband measurements performed during joint ACLOUD (Arctic CLoud Observations Using airborne polar Day) PASCAL (Physical feedbacks boundary layer, Sea ice, Cloud AerosoL) campaigns, which were in May–June 2017 north Svalbard. The SIS tested using measured quantities prognostic...

10.5194/tc-13-1695-2019 article EN cc-by ˜The œcryosphere 2019-06-26

Abstract. This case study explores the evolution of clouds during an Arctic cold air outbreak in Fram Strait region observed HALO-(𝒜𝒞)3 aircraft campaign. Our research provides information about formation, structure, micro- and macrophysical properties, radiative effects investigates role vertical wind shear buoyancy forces transition from regular cloud streets to rather isotropic patterns. findings show that lower horizontal boundary layer speeds (< 12 m s-1) disrupt formation streets,...

10.5194/egusphere-2025-201 preprint EN cc-by 2025-01-28

Vegetation indices (VIs) derived from ground-based or unmanned aerial vehicle measurements use relative reflectance obtained by flying over well-defined panels (RP). The RP overflights provide a form of transfer calibration to determine reflectances the actual vegetated areas. It is assumed that environmental conditions, i.e., solar zenith angle (SZA) and cloud optical thickness (COT), remain constant between overflights. During typical 10-minute intervals overflights, COT varies especially...

10.5194/egusphere-egu25-1900 preprint EN 2025-03-14

Abstract. The HALO–(𝒜𝒞)3 aircraft campaign was carried out in March and April 2022 over the Norwegian Greenland seas, Fram Strait, central Arctic Ocean. Three research – High Altitude Long Range Research Aircraft (HALO), Polar 5, 6 performed 54 partly coordinated flights on 23 flight days areas of open ocean, marginal sea ice zone (MIZ), ice. general objective to quantify evolution air mass properties during moist warm-air intrusions (WAIs) cold-air outbreaks (CAOs). To obtain a...

10.5194/essd-17-1295-2025 article EN cc-by Earth system science data 2025-04-01

Abstract. In September 2002, the first INSPECTRO campaign to study influence of clouds on spectral actinic flux in lower troposphere was carried out East Anglia, England. Measurements flux, irradiance and aerosol cloud properties were made from four ground stations by aircraft. The radiation measurements modelled using uvspec model ancillary data. For cloudless conditions, reproduced 1-D radiative transfer modelling within measurement uncertainties about ±10%. overcast days, ground-based...

10.5194/acp-5-1975-2005 article EN cc-by-nc-sa Atmospheric chemistry and physics 2005-08-03

Abstract. Arctic summer sea ice experiences rapid changes in its sea-ice concentration, surface albedo, and the melt pond fraction. This affects energy balance of region demands an accurate knowledge those characteristics climate models. In this paper, broadband albedo (300–3000 nm) is derived from MEdium Resolution Imaging Spectrometer (MERIS) optical swath data by transforming spectral as output Melt Pond Detector (MPD) algorithm with a newly developed spectral-to-broadband conversion...

10.5194/tc-14-165-2020 article EN cc-by ˜The œcryosphere 2020-01-22

Abstract. The surface reflection of solar radiation comprises an important boundary condition for radiative transfer simulations. In polar regions above snow surfaces, the is particularly anisotropic due to low Sun elevations and highly scattering phase function crystals. characterization this anisotropy essential satellite remote sensing over both Arctic Antarctica. To quantify angular properties, hemispherical-directional reflectance factor (HDRF) surfaces was derived from airborne...

10.5194/tc-14-3959-2020 article EN cc-by ˜The œcryosphere 2020-11-12
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