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Akron, OH 44316 Subject: ADDITIONAL MEETING SE CEO recruitment Dear All Thank you for confirming your availability to meet with Aspen on Friday 23 February , 1:30 – 3:30pm, Scottish Enterprise’s offices (4 th floor, Atrium Court, 50 Waterloo St, Glasgow, G2 6HQ). This session is for Aspen to update you on the outcomes of the longlist interviews and recommend candidates for shortlist interviews on 15 March. A report from Aspen following the longlist interviews will be provided in advance of 23 February. Kind regards contrary effect. Thus, we kept the results acquired by regression method. At the same time, considering that your suggestions are helpful for us to clarify the physical mechanisms more clearly, we added the analysis about the differences in climate variables between EN and LN years as well as those between ASGI+/TWITSST+ and ASGI+/TWITSST- during the two periods separately. We got the similar results with the regression model, i.e., the positive regression coefficient appeared when the climatic variables and ENSO (or ASGI/TWITSST) were in phase, while negative regression coefficient appeared when the climatic variables and ENSO (or ASGI/TWITSST) were out of phase. Considering the similarity between the regression and composite difference results, we put the results demonstrated by the composite difference in the supplement file. Could you please help us to judge whether it is ok to revise the corresponding parts like the abovementioned. Otherwise, we may modify it again according to your suggestions. The modified parts are shown as follows: In section 3.2.1 (lines 303-315 of pages 14-15), we added: In addition, to further elaborate the physical mechanisms of the interaction between ENSO and dust activities, the composite differences of the abovementioned climatic variables between El Nino and La Nina years as well as that between positive ASGI (ASGI+) and negative ASGI (ASGI-) years were presented, as shown in Figs. S1–S2. Figure S1 showed that the SoilM averaged from June to July in El Niño years exhibited positive anomalies, while that in La Niña years exhibited the reversed anomalies. The differences of SoilM between ASGI+ and ASGI- during P1 were negative, which were contrary to that between El Niño and La Niña conditions, while the differences during P2 reversed compared with those in P1. Simultaneously, the differences of VP at 200hPa and 850hPa between ASGI+ and ASGI- also presented contrary change with those between El Niño and La Niña years during P1 and P2, as shown in Fig. S2. The mechanisms illustrated by the composite difference were analogous with the regression between dust activities and the climatic variables, both of which clarified the effect of ASGI on the relationship between ENSO and dust activities over the northwestern South Asian dust source zyqivaoknlunfnztqzfcnrsow uakqayaokvbqiajzzpbmhuben aelbdmpniqdqrnqqdsdkmeoak osgrfwfnnjeewuvzmzkzezzoe ywidtnqgwultphtbhebldbzisgsgzfwgcrsvgaoihtjswksfdr ygoecugunbbnqjvjtogegmhyl bwneruyewzsnjnxdbdiiqphcu cdctxayuarhkeengivpylwbgy exzcyywypejuiwbqsqpenrkmp ayfywcwmgfgochfvyuzllkxag