All Stories

  1. The Reflectance Distribution of Shallow Cumulus and Its Environs From High Spatial Resolution ASTER Images
  2. Transient Darkening of Low‐Level Liquid Clouds by the 2022 Hunga Lamb Wave Observed in GOES‐R Imagery
  3. A GEO-GEO Stereo Observation of Diurnal Cloud Variations over the Eastern Pacific
  4. One‐Minute Resolution GOES‐R Observations of Lamb and Gravity Waves Triggered by the Hunga Tonga‐Hunga Ha'apai Eruptions on 15 January 2022
  5. Analysis of the Development of the Paroxysmal Eruption of the Sheveluch Volcano on April 10–13, 2023, Based on Data from Various Satellite Systems
  6. Quantifying the Impacts of the Angle of Attack on the Morphology of Atmospheric von Kármán Vortex Streets
  7. One-Minute Resolution GOES-R Observations of Lamb and Gravity Waves Triggered by the Hunga Tonga-Hunga Ha'apai Eruptions on 15 January 2022
  8. Quantifying the impacts of the angle of attack on the morphology of atmospheric von Kármán vortex stree
  9. Dispersion and Aging of Volcanic Aerosols After the La Soufrière Eruption in April 2021
  10. Analysis of the development of the paroxysmal eruption of Sheveluch volcano on April 10–13, 2023, based on data from various satellite systems
  11. Measurement report: Plume heights of the April 2021 La Soufrière eruptions from GOES-17 side views and GOES-16–MODIS stereo views
  12. Stereo Plume Height and Motion Retrievals for the Record‐Setting Hunga Tonga‐Hunga Ha'apai Eruption of 15 January 2022
  13. How the morning-afternoon cloudiness asymmetry affects the energy-maximizing azimuth direction of fixed-tilt monofacial solar panels
  14. Online treatment of eruption dynamics improves the volcanic ash and SO<sub>2</sub> dispersion forecast: case of the 2019 Raikoke eruption
  15. Stereo Plume Height and Motion Retrievals for the Record-Setting Hunga Tonga-Hunga Ha'apai Eruption of 15 January 2022
  16. Lagrangian Coherent Structures and Vortex Formation in High Spatiotemporal‐Resolution Satellite Winds of an Atmospheric Kármán Vortex Street
  17. Geometric estimation of volcanic eruption column height from GOES-R near-limb imagery – Part 1: Methodology
  18. Geometric estimation of volcanic eruption column height from GOES-R near-limb imagery – Part 2: Case studies
  19. Online treatment of eruption dynamics improves the volcanic ash and SO<sub>2</sub> dispersion forecast: case of the Raikoke 2019 eruption
  20. Lagrangian Coherent Structures and Vortex Formation in High Spatiotemporal-Resolution Satellite Winds of an Atmospheric Kármán Vortex Street
  21. Geometric estimation of volcanic eruption column height from GOES-R near-limb imagery – Part 1: Methodology
  22. Geometric estimation of volcanic eruption column height from GOES-R near-limb imagery – Part 2: Case studies
  23. Supplementary material to "Geometric estimation of volcanic eruption column height from GOES-R near-limb imagery – Part 1: Methodology"
  24. Supplementary material to "Geometric estimation of volcanic eruption column height from GOES-R near-limb imagery – Part 2: Case studies"
  25. The behavior of high-CAPE (convective available potential energy) summer convection in large-domain large-eddy simulations with ICON
  26. Using multi-scale modeling and observations to link the eruption source parameters to the dispersion of volcanic clouds in case of the Raikoke eruption 2019
  27. Sunflower inflorescences absorb maximum light energy if they face east and afternoons are cloudier than mornings
  28. Particle aging and aerosol–radiation interaction affect volcanic plume dispersion: evidence from the Raikoke 2019 eruption
  29. The behavior of high-CAPE summer convection in large-domain large-eddy simulations with ICON
  30. Particle Aging and Aerosol–Radiation Interaction Affect Volcanic Plume Dispersion: Evidence from Raikoke Eruption 2019
  31. The Research Unit VolImpact: Revisiting the volcanic impact on atmosphere and climate – preparations for the next big volcanic eruption
  32. Evolution of an Atmospheric Kármán Vortex Street From High‐Resolution Satellite Winds: Guadalupe Island Case Study
  33. Evolution of an atmospheric Kármán vortex street from high-resolution satellite winds: Guadalupe Island case study
  34. The Dependence of Shallow Cumulus Macrophysical Properties on Large‐Scale Meteorology as Observed in ASTER Imagery
  35. Evaluating the diurnal cycle of South Atlantic stratocumulus clouds as observed by MSG SEVIRI
  36. Characterizing the diurnal cycle of South Atlantic stratocumulus cloud properties from satellite retrievals
  37. Supplementary material to "Characterizing the diurnal cycle of South Atlantic stratocumulus cloud properties from satellite retrievals"
  38. Evaluation of the EUMETSAT Global AVHRR Wind Product
  39. Assessment of MISR Cloud Motion Vectors (CMVs) Relative to GOES and MODIS Atmospheric Motion Vectors (AMVs)
  40. High-resolution numerical modeling of mesoscale island wakes and sensitivity to static topographic relief data
  41. Testing a polarimetric cloud imager aboard research vessel Polarstern: comparison of color-based and polarimetric cloud detection algorithms
  42. View angle dependence of MODIS liquid water path retrievals in warm oceanic clouds
  43. Improvements to MISR stereo motion vectors
  44. CHASER: An Innovative Satellite Mission Concept to Measure the Effects of Aerosols on Clouds and Climate
  45. Comparison of MISR and Meteosat-9 cloud-motion vectors
  46. Global assessment of AMSR-E and MODIS cloud liquid water path retrievals in warm oceanic clouds
  47. Optics of sunlit water drops on leaves: conditions under which sunburn is possible
  48. Evaluation of passive satellite remote sensing of cloud liquid water
  49. Lagrangian Diagnostics of Tropical Deep Convection and Its Effect upon Upper-Tropospheric Humidity
  50. Cloud-fraction-dependent bias in satellite liquid water path retrievals of shallow, non-precipitating marine clouds
  51. Cloud motion vectors from MISR using sub-pixel enhancements
  52. Comparison of microwave and optical cloud water path estimates from TMI, MODIS, and MISR
  53. Why do dusk-active cockchafers detect polarization in the green? The polarization vision in Melolontha melolontha is tuned to the high polarized intensity of downwelling light under canopies during sunset
  54. Anisotropy of water cloud reflectance: A comparison of measurements and 1D theory
  55. Use of stereo-matching to coregister multiangle data from MISR
  56. Simultaneous retrieval of cloud motion and height from polar-orbiter multiangle measurements
  57. Feasibility and Error Analysis of Cloud Motion Wind Extraction from Near-Simultaneous Multiangle MISR Measurements
  58. Raindrops keep falling on my head