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Based on the normalized anomaly value, the number of warmer years predicted to be increasing.
But since the anomaly value changes rapidly for each received RREP, a malicious node can also recover very quickly from isolation phase.
That is, it determines the anomaly value by computing the ratio of number of actual routes established through that neighbour to the number of route replies transmitted by that neighbour.
WARP allows nodes to monitor the number of routes created through each neighbour and isolates a particular neighbour whose anomaly value (route-building rate) is greater than the threshold.
In the Ryukyu subduction zone, the entire fore-arc has a low anomaly value expect in the area where the LOFZ intersects the Ryukyu trench (approximately 125° E to 129° E; 23° N to 26.5° N) (Figure 2d).
Even though the route replies are not processed from such a neighbour whose anomaly value is greater than threshold, the route reply count maintained in the routing table for that neighbour is still incremented.
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Solid colored lines denote positive and negative PPR anomaly values.
When deepening, gravity anomaly is reduced, while when rising, gravity anomaly values increase.
Each node in WARP maintains the anomaly values of its neighbours in its routing table.
We are therefore left with a grid of 1,620,000 total intensity anomaly values.
In calculations of the gravity gradient tensor from the gravity anomaly, we need gravity anomaly values at different heights.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com