
In the given problem, we have a unique geographical configuration: an m x n rectangular island bordered on two edges by the Pacific Ocean and on the opposite two by the Atlantic Ocean. The Pacific touches the left and top edges, whereas the Atlantic touches the right and bottom edges. The island itself is divided into square cells which form a matrix, with each cell's value representing its height above sea level.
Rainfall on the island can lead to water traveling from one cell to adjacent ones, particularly directed to either or both oceans. However, there is a rule for the flow: water can move to a neighboring cell if and only if the neighboring cell's elevation is equal to or less than that of the current cell.
The challenge is to compute all the matrix coordinates [r, c] from which water can simultaneously reach both the Pacific and Atlantic oceans. These results are to be returned as a 2D list.
Input:
Output:
Explanation:
Input:
Output:
Explanation:
m == heights.lengthn == heights[r].length1 <= m, n <= 2000 <= heights[r][c] <= 105Initial Understanding:
[0, n-1] can drain directly to both the Pacific (from the top edge) and Atlantic (from the right edge).Travel Strategy:
pacificReachable and atlanticReachable.Common Cells Calculation:
pacificReachable and atlanticReachable are the answer, as they can drain into both oceans.By following the above methodologies, the problem can be approached logically, maintaining efficiency even as the matrix size scales to its upper limits as governed by the given constraints. The essence of the solution lies in effectively mapping water flow paths from the edges inwards, ensuring every possible path is accounted for by adapting typical graph traversal strategies.
The provided Java solution tackles the problem of identifying points in a grid where water can flow both to the Pacific and Atlantic oceans. Here's the breakdown of how this solution works:
totalRows and totalCols based on input grid dimensions, and a heights array to store the grid values.canReachPacific and canReachAtlantic—track whether each cell is reachable from the respective ocean.depthFirstSearch function recursively explores neighboring cells. It marks a cell as true in the relevant ocean matrix if the cell hasn't been visited and its height is higher or equal to the current cell—ensuring water can only flow from high to equal or lower height.Results are aggregated and returned as a list of lists, where each inner list contains the row and column indices of a valid cell. This method effectively and efficiently finds all required points in the grid with the potential of water flow to both oceans employing the DFS logical framework.
Solution Summary:
The provided Python3 code defines a solution to determine the cells in a matrix that can flow water to both the Pacific and Atlantic oceans. The matrix represents elevations, and water can only flow to lower or equal height neighbors.
pacific and atlantic sets to track cells that can reach respective oceans.traverse to perform a depth-first search (DFS) starting from given coordinates. This function adds the current cell to the visited set and then iterates over the four possible directions (right, down, left, up). It checks:traverse for the new position.The solution efficiently explores all possible paths from the ocean-bound cells inward, marking those that can send water back to the ocean. By using sets for both oceans, it ensures that the results are unique and calculates the common cells using set intersection, reducing computational complexity.
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