Abstract

The sub-daily variability of aerosols affects the estimates of daily mean aerosol loading. However, large spatial scale estimates of their climate effects are mostly based on snapshots from low orbit satellites that may bias the mean estimate for daily, monthly, or annual timescales. In this study, an attempt is made to estimate the magnitude of such bias based on ground and satellite-based datasets. Using ground-based measurements, we show an apparent asymmetry (of the order of 10–50%) in the sub-daily variability of aerosol loading over the Indian region. For the first time, it is reported that this sub-daily variability has a spatial pattern with an increasing amplitude toward the east of the subcontinent. We also find this variability in aerosol loading is well-captured by the satellites but with a lower amplitude. Our study shows that such differences could alter the annual surface radiative forcing estimates by more than ∼15 W m−2 over this region. We find that NASA’s Modern-Era Retrospective analysis for Research and Applications version 2 (MERRA-2), a state-of-the-art model-based chemical reanalysis, is unable to capture these sub-daily variabilities. This implies that both model and satellite-based radiative forcing estimates for large spatial scales should improve aerosol sub-daily information/variabilities for obtaining reliable radiative forcing estimates.

Highlights

  • The importance of atmospheric aerosols and their influence on climate are well-known

  • Similar analysis using satellite datasets reveals spatially such estimates could be ∼20%. These differences appear to be driven in part by the gradient in relative humidity

  • The nonaccountability of aerosol sub-daily variations can lead to substantial error in diurnally averaged or daily, seasonal, or annual forcing estimates

Read more

Summary

INTRODUCTION

The importance of atmospheric aerosols and their influence on climate are well-known. Since the Earth Observation Satellite era, low orbit satellites and their data have provided significant insights into large-scale features of aerosol distribution, transport, and variability at different timescales Due to their orbital characteristics, most insights are based on a few snapshots available within a day. This study attempts to elucidate the sub-daily variability of aerosols using ground and satellite-based aerosol optical depth measurements and their impact on the radiative effect over the Indian region. The annual and seasonal variability of ADR and SDR is computed to show the daytime (hereafter called sub-daily) variation of aerosol loading spatially over the Indian region. Multiplying the daily, seasonal/ annual averaged ARFE with ADR (ΔAOD from observations) SDR (ΔAOD form satellites) will provide ARF difference due to sub-daily/diurnal variability. Only the top of the atmosphere (TOA) forcing estimates are used in this study to elucidate forcing differences induced by sub-daily variability in aerosol loading

RESULT
SUMMARY AND CONCLUSION
DATA AVAILABILITY STATEMENT
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call