In situ and satellite-based estimates of cloud properties and aerosol–cloud interactions over the southeast Atlantic Ocean

oleh: S. Gupta, S. Gupta, S. Gupta, G. M. McFarquhar, G. M. McFarquhar, J. R. O'Brien, J. R. O'Brien, M. R. Poellot, D. J. Delene, I. Chang, L. Gao, F. Xu, J. Redemann

Format: Article
Diterbitkan: Copernicus Publications 2022-10-01

Deskripsi

<p>In situ cloud probe data from the NASA ObseRvations of Aerosols above CLouds and their intEractionS (ORACLES) field campaign were used to estimate the effective radius (<span class="inline-formula"><i>R</i><sub>e</sub></span>), cloud optical thickness (<span class="inline-formula"><i>τ</i></span>), and cloud droplet concentration (<span class="inline-formula"><i>N</i><sub>c</sub></span>) for marine stratocumulus over the southeast Atlantic Ocean. The in situ <span class="inline-formula"><i>R</i><sub>e</sub></span>, <span class="inline-formula"><i>τ</i></span>, and <span class="inline-formula"><i>N</i><sub>c</sub></span> were compared with co-located Moderate Resolution Imaging Spectroradiometer (MODIS) retrievals of <span class="inline-formula"><i>R</i><sub>e</sub></span> and <span class="inline-formula"><i>τ</i></span> and MODIS-derived <span class="inline-formula"><i>N</i><sub>c</sub></span>. For 145 cloud profiles, a MODIS retrieval was co-located with in situ data with a time gap of less than 1 h. On average, the MODIS <span class="inline-formula"><i>R</i><sub>e</sub></span> and <span class="inline-formula"><i>τ</i></span> (11.3 <span class="inline-formula">µ</span>m and 11.7) were 1.6 <span class="inline-formula">µ</span>m and 2.3 higher than the in situ <span class="inline-formula"><i>R</i><sub>e</sub></span> and <span class="inline-formula"><i>τ</i></span> with Pearson's correlation coefficients (<span class="inline-formula"><i>R</i></span>) of 0.77 and 0.73, respectively. The average MODIS <span class="inline-formula"><i>N</i><sub>c</sub></span> (151.5 cm<span class="inline-formula"><sup>−3</sup></span>) was within 1 cm<span class="inline-formula"><sup>−3</sup></span> of the average in situ <span class="inline-formula"><i>N</i><sub>c</sub></span> with an <span class="inline-formula"><i>R</i></span> of 0.90.</p> <p>The 145 cloud profiles were classified into 67 contact profiles where an aerosol concentration (<span class="inline-formula"><i>N</i><sub>a</sub></span>) greater than 500 cm<span class="inline-formula"><sup>−3</sup></span> was sampled within 100 m above cloud tops and 78 separated profiles where <span class="inline-formula"><i>N</i><sub>a</sub></span> less than 500 cm<span class="inline-formula"><sup>−3</sup></span> was sampled up to 100 m above cloud tops. Contact profiles had a higher in situ <span class="inline-formula"><i>N</i><sub>c</sub></span> (by 88 cm<span class="inline-formula"><sup>−3</sup></span>), higher <span class="inline-formula"><i>τ</i></span> (by 2.5), and lower in situ <span class="inline-formula"><i>R</i><sub>e</sub></span> (by 2.2 <span class="inline-formula">µ</span>m) compared to separated profiles. These differences were associated with aerosol–cloud interactions (ACI), and MODIS estimates of the differences were within 5 cm<span class="inline-formula"><sup>−3</sup></span>, 0.5, and 0.2 <span class="inline-formula">µ</span>m of the in situ estimates when profiles with MODIS <span class="inline-formula"><i>R</i><sub>e</sub><i>&gt;</i>15</span> <span class="inline-formula">µ</span>m or MODIS <span class="inline-formula"><i>τ</i><i>&gt;</i>25</span> were removed. The agreement between MODIS and in situ estimates of changes in <span class="inline-formula"><i>R</i><sub>e</sub></span>, <span class="inline-formula"><i>τ</i></span>, and <span class="inline-formula"><i>N</i><sub>c</sub></span> associated with ACI was driven by small biases in MODIS retrievals of cloud properties relative to in situ measurements across different aerosol regimes. Thus, when combined with estimates of aerosol location and concentration, MODIS retrievals of marine stratocumulus cloud properties over the southeast Atlantic can be used to study ACI over larger domains and longer timescales than possible using in situ data.</p>