... | @@ -17,13 +17,13 @@ Fig. 1: Time series of Arctic sea-ice area in (a) March and (b) September. The t |
... | @@ -17,13 +17,13 @@ Fig. 1: Time series of Arctic sea-ice area in (a) March and (b) September. The t |
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Fig. 2: Time series of Arctic sea-ice volume in (a) March and (b) September. The thick dashed black curve is the multi-model mean, the grey shading is +/- 10,000 km^3 around the multi-model mean, and the thick solid black curve is the PIOMAS reanalysis dataset. The number in brackets indicates the number of members to compute the mean sea-ice volume for each model (number of models for the multi-model mean).
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Fig. 2: Time series of Arctic sea-ice volume in (a) March and (b) September. The thick dashed black curve is the multi-model mean, the grey shading is +/- 10,000 km^3 around the multi-model mean, and the thick solid black curve is the PIOMAS reanalysis dataset. The number in brackets indicates the number of members to compute the mean sea-ice volume for each model (number of models for the multi-model mean).
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Fig. 3: Latitudinal transect of northward Atlantic ocean heat transport averaged over 2000-2014. The thick solid line is the reanalysis from Trenberth and Fasullo (2017) and the different dots show the hydrographic measurements with their associated uncertainty represented as error bars. The number in brackets indicates the number of members to compute the mean sea-ice area for each model.
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Fig. 3: Latitudinal transect of northward Atlantic ocean heat transport (OHT) averaged over 2000-2014. The thick solid line is the reanalysis from Trenberth and Fasullo (2017) and the different dots show the hydrographic measurements with their associated uncertainty represented as error bars. The number in brackets indicates the number of members to compute the mean OHT for each model.
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Fig. 4: Latitudinal transect of northward Pacific ocean heat transport averaged over 2000-2014. The number in brackets indicates the number of members to compute the mean sea-ice area for each model.
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Fig. 4: Latitudinal transect of northward Pacific ocean heat transport (OHT) averaged over 2000-2014. The number in brackets indicates the number of members to compute the mean OHT for each model.
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Fig. 5: Time series of northward Atlantic ocean heat transport at (a) 60N and (b) 70N. The number in brackets indicates the number of members to compute the mean sea-ice area for each model.
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Fig. 5: Time series of northward Atlantic ocean heat transport (OHT) at (a) 60N and (b) 70N. The number in brackets indicates the number of members to compute the mean OHT for each model.
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Fig. 6: Scatter plots of detrended March Arctic sea-ice area against detrended annual mean Atlantic ocean heat transport for all points between 1950 and 2014 and for the 9 best models in terms of Arctic SIA, SIV and Atlantic OHT. The correlation coefficients *R* and regression slopes *a* (unit: 1000 km^2 per TW) are shown in the upper right corner of each panel for each model.
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Fig. 6: Scatter plots of detrended March Arctic sea-ice area against detrended annual mean Atlantic ocean heat transport for all points between 1950 and 2014 and for the 9 best models in terms of Arctic SIA, SIV and Atlantic OHT. The correlation coefficients *R* and regression slopes *a* (unit: 1000 km^2 per TW) are shown in the upper right corner of each panel for each model.
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