Figures & data
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Figure 1. Normalized time series of the PJ and MnE indices during summer over the period 1958–2016. Solid lines indicate the +0.5/−0.5 standard deviations.
![Figure 1. Normalized time series of the PJ and MnE indices during summer over the period 1958–2016. Solid lines indicate the +0.5/−0.5 standard deviations.](/cms/asset/fb38f561-8799-410c-ad3b-ee2ad35f41db/taos_a_1585101_f0001_c.jpg)
Figure 2. Regressed geopotential height (shading; units: gpm) and wind (vectors; units: m s−1) anomalies at (a) 850 hPa, (b) 500 hPa, and (c) 200 hPa against the PJ index during summer over the period 1958–2016. (d–f) As in (a–c) but against the MnE index. The dotted areas are geopotential height anomalies significant at the 95% confidence level. Arrows are the wind anomalies significant at the 95% confidence level. The green box in Figure 2(d) represents the domain used to define the MnE index.
![Figure 2. Regressed geopotential height (shading; units: gpm) and wind (vectors; units: m s−1) anomalies at (a) 850 hPa, (b) 500 hPa, and (c) 200 hPa against the PJ index during summer over the period 1958–2016. (d–f) As in (a–c) but against the MnE index. The dotted areas are geopotential height anomalies significant at the 95% confidence level. Arrows are the wind anomalies significant at the 95% confidence level. The green box in Figure 2(d) represents the domain used to define the MnE index.](/cms/asset/f9ea336c-d23c-4f45-83aa-e4e8f2d8cd72/taos_a_1585101_f0002_c.jpg)
Figure 3. Regression maps of the total radiation flux (units: W m−2) against the (a) PJ and (b) MnE indices during summer over the period 1958–2016. (c, d) As in (a, b) but for the SAT (units: °C). The dotted areas are significant at the 95% confidence level.
![Figure 3. Regression maps of the total radiation flux (units: W m−2) against the (a) PJ and (b) MnE indices during summer over the period 1958–2016. (c, d) As in (a, b) but for the SAT (units: °C). The dotted areas are significant at the 95% confidence level.](/cms/asset/9cb39750-d508-478d-bbe6-704e940ea55e/taos_a_1585101_f0003_c.jpg)
Table 1. List of +PJ/+MnE, +PJ/−MnE, −PJ/+MnE, and −PJ/−MnE years over the period 1958–2016.
Figure 4. Composite differences in the geopotential height (units: gpm) and wind (vectors; units: m s−1) at (a) 850 hPa, (b) 500 hPa, and (c) 200 hPa between the +PJ/+MnE and −PJ/−MnE years during summer over the period 1958–2016. (d–f) As in (a–c) but between the +PJ/−MnE and +PJ/−MnE years. The dotted areas are geopotential height anomalies significant at the 95% confidence level. Arrows are the wind anomalies significant at the 95% confidence level.
![Figure 4. Composite differences in the geopotential height (units: gpm) and wind (vectors; units: m s−1) at (a) 850 hPa, (b) 500 hPa, and (c) 200 hPa between the +PJ/+MnE and −PJ/−MnE years during summer over the period 1958–2016. (d–f) As in (a–c) but between the +PJ/−MnE and +PJ/−MnE years. The dotted areas are geopotential height anomalies significant at the 95% confidence level. Arrows are the wind anomalies significant at the 95% confidence level.](/cms/asset/b02a2d25-486b-4f16-9019-668231ccbdc5/taos_a_1585101_f0004_c.jpg)
Figure 5. Composite differences in the SAT (units: °C) (a) between the +PJ/+MnE and −PJ/−MnE years and (b) between the +PJ/−MnE and −PJ/+MnE years during summer over the period 1958–2016. The dotted areas are significant at the 95% confidence level.
![Figure 5. Composite differences in the SAT (units: °C) (a) between the +PJ/+MnE and −PJ/−MnE years and (b) between the +PJ/−MnE and −PJ/+MnE years during summer over the period 1958–2016. The dotted areas are significant at the 95% confidence level.](/cms/asset/d100931f-ee5f-4fc1-b79d-4d165a4ab773/taos_a_1585101_f0005_c.jpg)