
The task revolves around calculating the volume of water trapped on a 2D topographic map after rainfall. Specifically, we are given a matrix named heightMap where each element represents the elevation of a square unit cell of the terrain. The goal is to calculate the total volume of water that remains trapped between the elevated regions of the map post-rain. The matrix dimensions, m x n, depict the size of the elevation map. This computational challenge involves dealing with spatial structures on a grid and determining the interaction between them when subjected to water accumulation scenarios.
Input:
Output:
Explanation:
Input:
Output:
m == heightMap.lengthn == heightMap[i].length1 <= m, n <= 2000 <= heightMap[i][j] <= 2 * 104Understanding the water trapping on a 2D map can be visualized similar to a 3D landscape where rain falls uniformly over the area. Post-rain, some areas of the map, depending on their surrounding elevation, will collect and hold water. Here's how we can intuit the process:
Example Interpretations based on the examples provided:
[[1,4,3,1,3,2], [3,2,1,3,2,4], [2,3,3,2,3,1]], visualize a small basin where there are pockets (depicted by lower numbers surrounded by higher numbers). After simulating rain, these pockets trap water. The volume, in this case, was calculated as 4 units.1 and surrounded by walls of 3s, the water trapped is greater. The calculation provided the trapped volume as 10 units, showcasing a more extensive central pool.These examples adhere strictly to the constraints that the matrix is at least 1x1 and at most 200x200 with the heights of each cell ranging from 0 to 20000, ensuring that computations remain manageable yet potentially detailed and complex depending on the landscape given.
This solution addresses the problem of computing the volume of water that can be trapped in a 3D landscape represented by a 2D elevation map. The algorithm employs a priority queue (min-heap) to dynamically select the lowest boundary on the surface, and a breadth-first search strategy to visit and calculate trapped water for each cell. The solution is implemented in C++ and outlined below:
WaterCell, which stores a cell's height along with its row and column index.This approach not only systematically expands the boundary inward but also ensures that the lowest edges are processed first, thus maximizing the trapped water calculation by making optimal local decisions that lead to the global optimum.
0 Comments
Be the first to comment and share your perspective with the community.