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At line 3, with the movement from up to down in the lattice, starting at node S, when considering a node N for which one of the conditions in (^{({M})}) has been violated, we eliminate all sub-branches of N and supplement N into the negative border of the sub-lattice containing the class (mathrm{FCS}_{C_0 subseteq C_1 } ( {s_0^{prime },s_1^{prime }})).
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For instance, with the monotonic property (supp(L) (le {s}_1^{prime }) and L supseteq {C}_0 )^{({M})}), we illustrate the creation of negative border in the algorithm as follows.
It is important to note that, from the Hass diagram on the lattice (mathcal {LCG}), if the concepts of positive and negative borders [23], concerning the anti-monotonic and monotonic properties of the support and item constraints, are added to the algorithm, then the sub-lattices whose closed itemsets satisfy the corresponding constraints will be generated quickly.
The lowest temperatures are bound to the negative thermal anomalies at the southern border of the model area (~10 °C) and to the negative thermal anomaly predicted in the south-east of Munich (up to 15 °C).
The negative thermal anomaly at the southern border of the model area decreased strongly in size and predicted temperatures are about 50 °C.
The negative thermal anomalies along the southern border of the model area decrease in size and show low temperatures of up to 20 °C.
These effects may partly explain the positive thermal anomalies around Munich and at the eastern border of Bavaria with a negative thermal anomaly in between.
Results ("raw" and "normalized" classification images) are shown in figure 4. Classification images peak inside the border of the patch and have negative peaks in the background, next to the border.
Classification images for three subjects are presented in figure 5. Classification images reveals positive peaks inside the border of the patch and less prominent negative peaks in the background immediately next to the border.
Note that a positive value for meniscal extrusion indicates an "external" position relative to the external border of the tibial plateau, whereas a negative value indicates an "internal" position relative to the external border.
At this depth, the coldest temperatures are limited to the negative thermal anomalies in the Folded Molasse Sediments at the southern border of the model area.
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