Microtopo specialist: 3DEP elevation + TWI + HAND
Browse filesUSGS 3DEP 1/3 arcsec DEM (resampled to 30 m for runtime), with two
hydrology indices computed offline by whitebox-workflows:
TWI — topographic wetness, ln(a/tan β), high where flow accumulates
HAND — height above nearest drainage, low where overbank flooding
pools first
These three rasters give the briefing terrain context that the
empirical/forward-modelled flood layers can't: even a parcel outside
every published zone can be in a topographic sink that any heavy rain
will fill.
.gitattributes routes *.tif through LFS.
- .gitattributes +1 -0
- app/context/microtopo.py +208 -0
- data/hand.tif +3 -0
- data/nyc_dem_30m.tif +3 -0
- data/twi.tif +3 -0
.gitattributes
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# Riprap-specific LFS tracking
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*.geojson filter=lfs diff=lfs merge=lfs -text
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# Esri FileGDB internal binary files (DEP Stormwater scenario data)
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*.gdbtable filter=lfs diff=lfs merge=lfs -text
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# Riprap-specific LFS tracking
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*.geojson filter=lfs diff=lfs merge=lfs -text
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*.tif filter=lfs diff=lfs merge=lfs -text
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# Esri FileGDB internal binary files (DEP Stormwater scenario data)
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*.gdbtable filter=lfs diff=lfs merge=lfs -text
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app/context/microtopo.py
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"""LiDAR/DEM-derived micro-topography specialist.
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Reads a window from a precomputed NYC-wide DEM (data/nyc_dem_30m.tif)
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fetched from USGS 3DEP via py3dep. Computes per-address terrain numbers
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that the static FEMA/DEP scenario maps don't expose.
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Metrics (all derived from the same small AOI raster):
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point_elev_m elevation at the address (m)
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rel_elev_pct_750m percentile of point elev in a 750-m radius
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rel_elev_pct_200m percentile of point elev in a 200-m radius
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(block-scale "is this a bowl?")
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basin_relief_m max-elev in 750-m AOI minus point elev
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aoi_min_m, aoi_max_m for context
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resolution_m
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We deliberately stop at "shape-of-the-terrain" metrics rather than full
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hydrology — depression-fill / D8 flow accumulation on a flat coastal
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DEM are noisy and slow. Percentile + relief is what the reconciler
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actually needs to write a useful sentence.
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"""
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from __future__ import annotations
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import logging
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import warnings
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from dataclasses import dataclass
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from pathlib import Path
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import numpy as np
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warnings.filterwarnings("ignore")
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log = logging.getLogger("riprap.microtopo")
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DOC_ID = "microtopo"
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CITATION = "USGS 3DEP 30 m DEM (precomputed citywide GeoTIFF, WGS84)"
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DATA_DIR = Path(__file__).resolve().parent.parent.parent / "data"
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DEM_PATH = DATA_DIR / "nyc_dem_30m.tif"
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TWI_PATH = DATA_DIR / "twi.tif"
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HAND_PATH = DATA_DIR / "hand.tif"
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@dataclass
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class Microtopo:
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point_elev_m: float
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rel_elev_pct_750m: float # 0..100
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rel_elev_pct_200m: float # 0..100
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basin_relief_m: float
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aoi_min_m: float
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aoi_max_m: float
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aoi_radius_m: int
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resolution_m: int
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# Hydrology indices computed on the same DEM (whitebox-workflows)
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twi: float | None = None # Topographic Wetness Index, ln(SCA / tan(slope))
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hand_m: float | None = None # Height Above Nearest Drainage (m)
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def _percentile_in_window(arr: np.ndarray, iy: int, ix: int, point_val: float,
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window_radius_cells: int) -> float:
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H, W = arr.shape
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y0 = max(0, iy - window_radius_cells)
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y1 = min(H, iy + window_radius_cells + 1)
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x0 = max(0, ix - window_radius_cells)
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x1 = min(W, ix + window_radius_cells + 1)
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sub = arr[y0:y1, x0:x1]
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finite = sub[np.isfinite(sub)]
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if finite.size == 0:
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return float("nan")
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return float((finite < point_val).sum()) / finite.size * 100.0
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_DEM_CACHE: dict = {}
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def _read_full_raster(path: Path) -> tuple[np.ndarray | None, dict | None]:
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import rasterio
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if not path.exists():
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return None, None
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with rasterio.open(path) as ds:
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arr = ds.read(1).astype("float32")
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nodata = ds.nodata
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meta = {"H": ds.height, "W": ds.width,
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"transform": ds.transform, "crs": ds.crs, "nodata": nodata}
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if nodata is not None:
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arr = np.where(arr == nodata, np.nan, arr)
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return arr, meta
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def _load_dem():
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"""Read the precomputed NYC DEM + TWI + HAND rasters into memory.
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All three are aligned (same grid, same transform). We hold them as
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numpy arrays so per-query slicing is safe under threading.
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"""
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if "arr" in _DEM_CACHE:
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return _DEM_CACHE
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arr, meta = _read_full_raster(DEM_PATH)
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if arr is None:
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log.warning("microtopo DEM not found at %s — run scripts/fetch_nyc_dem.py", DEM_PATH)
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return None
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twi, _ = _read_full_raster(TWI_PATH)
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hand, _ = _read_full_raster(HAND_PATH)
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_DEM_CACHE.update({
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"arr": arr, "H": meta["H"], "W": meta["W"],
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"transform": meta["transform"], "crs": meta["crs"],
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"twi": twi, "hand": hand,
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})
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note = []
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if twi is not None: note.append(f"TWI {TWI_PATH.name}")
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if hand is not None: note.append(f"HAND {HAND_PATH.name}")
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log.info("microtopo: loaded NYC DEM %s (%dx%d, %s); aux: %s",
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DEM_PATH.name, meta["H"], meta["W"], meta["crs"],
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", ".join(note) if note else "(none — algorithmic only)")
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return _DEM_CACHE
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def warm():
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_load_dem()
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def _row_col(transform, lat: float, lon: float) -> tuple[int, int]:
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"""Inverse-affine: WGS84 (lon,lat) -> raster (row, col).
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Mirrors rasterio.transform.rowcol but without holding a dataset handle.
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"""
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# affine: x = a*col + b*row + c ; y = d*col + e*row + f
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# invert: col = (a_inv * (x - c)) approx — we have a diagonal affine
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a, b, c, d, e, f = transform.a, transform.b, transform.c, transform.d, transform.e, transform.f
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# diagonal case (b=d=0, common for north-up rasters):
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col = int(round((lon - c) / a))
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row = int(round((lat - f) / e))
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return row, col
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def microtopo_at(lat: float, lon: float, radius_m: int = 750) -> Microtopo | None:
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state = _load_dem()
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if state is None:
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return None
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arr_full = state["arr"]
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transform = state["transform"]
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try:
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row, col = _row_col(transform, lat, lon)
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except Exception as e:
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log.warning("microtopo index failed: %s", e)
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return None
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res_m = abs(transform.a) * 111_000.0 * np.cos(np.radians(lat))
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cells_radius = max(2, int(np.ceil(radius_m / max(res_m, 1.0))))
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H, W = state["H"], state["W"]
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y0 = max(0, row - cells_radius); y1 = min(H, row + cells_radius + 1)
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x0 = max(0, col - cells_radius); x1 = min(W, col + cells_radius + 1)
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if y1 <= y0 or x1 <= x0:
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return None
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arr = arr_full[y0:y1, x0:x1].copy()
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iy = row - y0
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ix = col - x0
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if not (0 <= iy < arr.shape[0] and 0 <= ix < arr.shape[1]):
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return None
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point_elev = float(arr[iy, ix])
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if not np.isfinite(point_elev):
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for r in range(1, 6):
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ya, yb = max(0, iy - r), min(arr.shape[0], iy + r + 1)
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xa, xb = max(0, ix - r), min(arr.shape[1], ix + r + 1)
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sub = arr[ya:yb, xa:xb]
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if np.isfinite(sub).any():
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point_elev = float(np.nanmean(sub))
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break
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else:
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return None
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finite = arr[np.isfinite(arr)]
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if finite.size == 0:
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return None
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aoi_min = float(finite.min())
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aoi_max = float(finite.max())
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pct_750 = float((finite < point_elev).sum()) / finite.size * 100.0
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cells_200m = max(1, int(round(200 / max(res_m, 1.0))))
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pct_200 = _percentile_in_window(arr, iy, ix, point_elev, cells_200m)
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twi_arr = state.get("twi")
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hand_arr = state.get("hand")
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twi_v: float | None = None
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hand_v: float | None = None
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if twi_arr is not None and 0 <= row < H and 0 <= col < W:
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v = float(twi_arr[row, col])
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twi_v = round(v, 2) if np.isfinite(v) else None
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if hand_arr is not None and 0 <= row < H and 0 <= col < W:
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v = float(hand_arr[row, col])
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hand_v = round(v, 2) if np.isfinite(v) else None
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return Microtopo(
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point_elev_m=round(point_elev, 2),
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rel_elev_pct_750m=round(pct_750, 1),
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rel_elev_pct_200m=round(pct_200, 1),
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basin_relief_m=round(aoi_max - point_elev, 2),
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aoi_min_m=round(aoi_min, 2),
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aoi_max_m=round(aoi_max, 2),
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aoi_radius_m=radius_m,
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resolution_m=int(round(res_m)),
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twi=twi_v,
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hand_m=hand_v,
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)
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data/hand.tif
ADDED
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Git LFS Details
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data/nyc_dem_30m.tif
ADDED
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Git LFS Details
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data/twi.tif
ADDED
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Git LFS Details
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