Publications

Peer-reviewed journal articles, manuscripts under review, and featured work.

Peer-Reviewed Publications

  1. A global decline in atmospheric dust during the 21st century. New 2026
    Ashok Kumar Gupta, J. F. Kok, V. Amiridis, A. Gkikas, K. Rizos, E. Proestakis, S. Logothetis, E. Marinou & C. Pérez García-Pando.
    Science Advances (2026). Preprint
  2. Desert dust exerts a substantial longwave radiative forcing missing from climate models. New 2026
    J. F. Kok, Ashok Kumar Gupta, A. T. Evan, A. A. Adebiyi, S. Albani, Y. Balkanski, R. Checa-Garcia, P. R. Colarco, D. Hamilton, Y. Huang, A. Ito, M. Klose, L. Li, N. M. Mahowald, R. L. Miller, V. Obiso, C. Pérez García-Pando, A. Rocha Lima & J. Wan.
    Nature Communications, 17: 3191 (2026). DOI
  3. The January 2022 Hunga eruption cooled the Southern Hemisphere in 2022 and 2023.
    Ashok Kumar Gupta, T. Mittal, K. Fauria, R. Bennartz & J. Kok.
    Communications Earth & Environment, 6: 240 (2025). DOI
  4. Eruption chronology of the December 2021 to January 2022 Hunga Tonga–Hunga Ha'apai eruption sequence.
    Ashok Kumar Gupta, R. Bennartz, K. E. Fauria & T. Mittal.
    Communications Earth & Environment, 3: 314 (2022). DOI
  5. The microphysics of warm-rain and ice-crystal processes of precipitation in simulated continental convective storms.
    Ashok Kumar Gupta, V. T. J. Phillips, D. Waman, S. Patade, A. Deshmukh, A. Jadav & A. Bansemer.
    Communications Earth & Environment, 4: 226 (2023). DOI
  6. Ash deposition triggers phytoplankton blooms at Nishinoshima Volcano, Japan.
    L. Kelly, K. Fauria, T. Mittal, J. El Kassar, R. Bennartz, D. Nicholson, A. Subramaniam & Ashok Kumar Gupta.
    Geochemistry, Geophysics, Geosystems, 24(11): e2023GC010914 (2023). DOI
  7. Simultaneous creation of a large vapor plume and pumice raft by the 2021 Fukutoku-Oka-no-Ba eruption.
    K. E. Fauria, M. Jutzeler, T. Mittal, Ashok Kumar Gupta, L. Kelly, J. Rausch, R. Bennartz, B. Delbridge & L. Retailleau.
    Earth and Planetary Science Letters, 118076 (2023).
  8. The influence of multiple biological ice-nucleating groups on mixed-phase clouds during MC3E.
    S. Patade, D. Waman, A. Deshmukh, A. Jadav, Ashok Kumar Gupta, V. T. J. Phillips, A. Bansemer, J. Carlin & A. Ryzhkov.
    Atmospheric Chemistry and Physics, 22(18): 12055–12075 (2022).
  9. Dependencies of secondary ice production on cloud-top temperature in a continental convective storm.
    D. Waman, S. Patade, A. Jadav, A. Deshmukh, Ashok Kumar Gupta, V. T. J. Phillips, A. Bansemer & P. J. DeMott.
    Journal of the Atmospheric Sciences, 79(12): 3375–3404 (2022).
  10. Multi-year diurnal variations of TOA cloud radiative forcing over the tropics from Megha-Tropiques-ScaRaB/3.
    Ashok Kumar Gupta, K. Rajeev, E. V. Davis, M. K. Mishra & A. K. M. Nair.
    Climate Dynamics, 55: 3289–3306 (2020). DOI
  11. Enhanced daytime occurrence of upper-tropospheric clouds over land and ocean.
    Ashok Kumar Gupta, K. Rajeev, S. Sijikumar & A. K. M. Nair.
    Atmospheric Research, 201: 133–143 (2018).
  12. Day–night changes in low-altitude cloud properties over stratocumulus-dominated oceans.
    Ashok Kumar Gupta, K. Rajeev & S. Sijikumar.
    Journal of Atmospheric and Solar-Terrestrial Physics, 161: 118–126 (2017). DOI
  13. Diurnal variation of shortwave aerosol direct radiative effect over dust-dominated regions.
    M. K. Mishra, Ashok Kumar Gupta & K. Rajeev.
    IEEE Trans. Geosci. Remote Sens., 55: 6610–6616 (2017). DOI

Under Review / Manuscripts in Preparation

  1. Organization of ice-multiplication mechanisms among basic cloud types — Part I: Validation and analysis of the control simulations.
    A. Deshmukh, D. Waman, S. Patade, M. Gautam, V. T. J. Phillips, A. Bansemer, Ashok Kumar Gupta, P. Connolly, G. McFarquhar, P. J. DeMott, J. Fan, Y. Lin, J. Schrod & H. Bingemer.
    Submitting to npj Climate and Atmospheric Science.
  2. Organization of ice-multiplication mechanisms among basic cloud types — Part II: Sensitivity tests.
    A. Deshmukh, D. Waman, S. Patade, Ashok Kumar Gupta & V. T. J. Phillips.
    Submitting to npj Climate and Atmospheric Science.
  3. Ice loading controls the vertical distribution of radiative heating in tropical cirrus. New 2026
    Ashok Kumar Gupta & R. Bennartz.
    Submitted to Proceedings of the National Academy of Sciences (PNAS).
  4. What's driving the global decline in mineral dust emissions during the early 21st century?
    Ashok Kumar Gupta, J. F. Kok, R. Bennartz, V. Amiridis, A. Gkikas, K. Rizos, E. Proestakis & C. Pérez García-Pando.
    In preparation; abstract submitted to the AMS Annual Meeting 2027.
  5. Umbrella-cloud growth and transport in explosive volcanic eruptions: Insights from the 2022 Hunga eruption and beyond.
    Ashok Kumar Gupta & R. Bennartz.
    In preparation.
  6. Deep learning-based temporal tracking of volcanic umbrella cloud properties from spaceborne sensors: The 2022 Hunga and 2024 Ruang eruptions.
    Ashok Kumar Gupta & R. Bennartz.
    Manuscript ready for submission (Remote Sensing of Environment).
  7. Model data from the AeroCom Dust Radiative Forcing from reconstructed dust changes since pre-industrial times experiment.
    O. W. Haugvaldstad, J. Kok, T. Storelvmo, M. Schulz, …, Ashok Kumar Gupta, et al.
    Under review (Geophysical Research Letters).

Featured Publications

Annual dust aerosol optical depth, 2003–2023, by region and globally

Earth has become less dusty in the 21st century

Gupta et al., 2026 · Science Advances

Year-to-year changes in dust aerosol optical depth (DAOD), a measure of atmospheric dustiness, from 2003 to 2023 across major dust-source regions and globally. Global DAOD declined by −10 ± 8 %, with decreases across much of the Northern Hemisphere; shaded ranges show estimate uncertainty.

Strongest evidence yet of a global dust decline.

Hunga cooling

Hunga eruption cooled the Southern Hemisphere

Gupta et al., 2025 · Comms Earth & Env

Net cooling of −0.55 W m⁻² from sulfate aerosols drove a −0.10 K SH temperature anomaly — contradicting warming projections.

Measurable volcanic cooling challenges climate projections.

ConvLSTM

ML-based volcanic umbrella cloud detection

Gupta & Bennartz · Manuscript ready

Deep-learning tracking of volcanic umbrella-cloud properties from geostationary satellite imagery, demonstrated on the 2022 Hunga and 2024 Ruang eruptions.

Toward rapid, automated ash-hazard monitoring.

Warm vs cold rain

Warm vs. cold rain in continental storms

Gupta et al., 2023 · Comms Earth & Env

Warm-rain processes account for ~80% of surface precipitation in very warm-based clouds.

Cloud-base warming shifts precipitation to warm-rain.

Hunga chronology

Volcanic umbrella clouds: Hunga Tonga

Gupta et al., 2022 · Comms Earth & Env

Unprecedented umbrella heights (~31 km), two ice-rich layers, volumetric flow of ~5.0 × 10¹¹ m³ s⁻¹.

Record-high volcanic clouds redefine eruption science.

Annual dust aerosol optical depth, 2003–2023, by region and globally

Earth has become less dusty in the 21st century

Gupta et al., 2026 · Science Advances

Year-to-year changes in dust aerosol optical depth (DAOD), a measure of atmospheric dustiness, from 2003 to 2023 across major dust-source regions and globally. Global DAOD declined by −10 ± 8 %, with decreases across much of the Northern Hemisphere; shaded ranges show estimate uncertainty.

Strongest evidence yet of a global dust decline.

Hunga cooling

Hunga eruption cooled the Southern Hemisphere

Gupta et al., 2025 · Comms Earth & Env

Net cooling of −0.55 W m⁻² from sulfate aerosols drove a −0.10 K SH temperature anomaly — contradicting warming projections.

Measurable volcanic cooling challenges climate projections.

ConvLSTM

ML-based volcanic umbrella cloud detection

Gupta & Bennartz · Manuscript ready

Deep-learning tracking of volcanic umbrella-cloud properties from geostationary satellite imagery, demonstrated on the 2022 Hunga and 2024 Ruang eruptions.

Toward rapid, automated ash-hazard monitoring.

Warm vs cold rain

Warm vs. cold rain in continental storms

Gupta et al., 2023 · Comms Earth & Env

Warm-rain processes account for ~80% of surface precipitation in very warm-based clouds.

Cloud-base warming shifts precipitation to warm-rain.

Hunga chronology

Volcanic umbrella clouds: Hunga Tonga

Gupta et al., 2022 · Comms Earth & Env

Unprecedented umbrella heights (~31 km), two ice-rich layers, volumetric flow of ~5.0 × 10¹¹ m³ s⁻¹.

Record-high volcanic clouds redefine eruption science.