Nepal GLOF Exposure LensMethodology & sources

How the screening works

This application is a transparent exposure-screening tool. It identifies hydrologically connected relationships between glacial lakes and hydropower project points along the mapped river network. It is not a hydrodynamic GLOF model and its scores are not probabilities.

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1. What this application measures

The core question is: does a hydropower project point lie downstream, on the same mapped HydroRIVERS network, of a glacial lake? When it does, the tool records the connection, estimates the downstream river-network distance, reports the lake's hazard evidence (ICIMOD expert rank where one exists, and observable GLO lake characteristics), and calculates transparent screening scores.

Important terminology

Hazard is the potentially dangerous lake/source. Exposure is the downstream hydrological relationship. Vulnerability describes how the project would respond to flood forces. Risk combines hazard, exposure, vulnerability and consequences. This application mainly establishes exposure and screening priority; it does not model vulnerability or expected loss.

2. Analysis modes: PDGLs Only and All GLOs

All projects, all GLO lakes and the ICIMOD PDGLs are always visible on the map. The analysis mode decides which lakes contribute to the exposure calculation and statistics:

ModeHazard sourcesHazard evidence used
PDGLs OnlyThe 47 ICIMOD (2020) potentially dangerous glacial lakes.ICIMOD expert hazard rank (I/II/III) plus GLO expansion evidence where the PDGL is confidently matched to a GLO lake. Identical rules to version 1.0.
All GLOsEvery GLO 2017–2024 lake (4150 in the analysis window), including the PDGLs.A common All-Lake hazard proxy built from observable evidence (size, 2017–2024 change, glacier-fed connectivity) plus extra points for ICIMOD expert classification where it exists.

An ordinary GLO lake is never presented as if ICIMOD had classified it: its panel reads “ICIMOD PDGL: NO · ICIMOD hazard rank: Not available”. In PDGLs Only mode, ordinary GLO lakes remain visible (dimmed) and can still be searched and opened; their panel explains that they are not part of the current calculation.

3. Data sources

PDGL

Potentially Dangerous Glacial Lakes (ICIMOD, 2020)

ICIMOD (2020), potentially dangerous glacial lakes in the Koshi, Gandaki and Karnali basins.

Open source reference ↗
GLO

Glacial Lake Observatory unique lakes, Sentinel-2 2017–2024

Glacial Lake Observatory (GLO), Sentinel-2 unique-lake dataset, 2017–2024 (ESSD, 2026).

Open source reference ↗
PROJECTS

Nepal hydropower licence register (administrator-maintained Google Sheet)

Hydropower project licences (survey, generation, operation) compiled in the project Google Sheet; refreshed by the administrator.

Open source reference ↗

Published build: 2026-10-06T20:50:45+00:00. Geographic dataset built: 2026-10-06T20:50:45+00:00. Project sheet snapshot fetched: 2026-10-06T20:50:42+00:00. Hydropower projects keep stable internal IDs (HP_000001, …) across sheet edits.

4. Building one lake inventory

  1. GLO lakes. Every GLO unique-lake record inside the analysis window is imported with its attributes (area, 2017–2024 expansion rate, uncertainty and significance, connectivity, elevation) and its outline. Outlines stored in a projected CRS (e.g. Albers Equal Area) are converted to longitude/latitude; the conversion is checked against the record's own coordinates.
  2. PDGL matching. Each ICIMOD PDGL is compared with nearby GLO lakes using distance, outline containment, lake-area similarity and country consistency. Matches are one-to-one. High = the PDGL point lies inside the GLO outline (or ≤ 1.5 km with similar area); Medium = ≤ 3.5 km with broadly similar area; otherwise Review.
  3. Merging. A High/Medium match merges the PDGL into its GLO lake, so one physical lake is one map object carrying both the ICIMOD classification and the GLO change evidence. A PDGL with only a Review candidate (or none) stays a separate ICIMOD record, and its GLO evidence is not used.

5. Lake → river → project method

  1. Regional river extraction. The Asia-wide HydroRIVERS shapefile is scanned; only reaches intersecting the Nepal/transboundary analysis window are kept.
  2. Lake connection hierarchy. Each lake is matched to its nearest HydroRIVERS reach. The distance is measured from the lake centroid and reduced by the lake's equivalent radius (√(area/π)), so large lakes are not penalised for their size.
    • Direct HydroRIVERS connection — reach within 8 km: High (≤ 3 km) or Medium (≤ 8 km). If the lake and the reach fall in different HydroBASINS Level-6 basins, the grade is lowered one step.
    • Catchment-supported connection — reach 8–20 km away and inside the same HydroBASINS Level-6 basin as the lake: graded Review and labelled as catchment-supported.
    • Unresolved — no defensible connection. No result is forced: unresolved lakes are shown but never contribute to exposure.
  3. Project snapping. Each project point is matched to its nearest reach (≤ 15 km) and the snap distance is stored and disclosed.
  4. Downstream tracing. From each connected lake's reach the engine follows HydroRIVERS NEXT_DOWN reach by reach. A project is connected only if its reach lies on that downstream chain. Links are stored once per build, so the public map only performs database look-ups.
  5. Flow-path distance. Estimated from HydroRIVERS downstream-distance attributes. It is a screening distance along the mapped network, not a simulated GLOF travel distance or arrival time.
Lake → matched HydroRIVERS reach → NEXT_DOWN → NEXT_DOWN → … → project reach

6. Connection confidence

A score says how strong the screening signal is; connection confidence says how certain the river connection itself is. They are reported separately. A link's confidence is the weakest of the lake connection, the project snap and the same-reach check.

GradeProject snapLake connectionMeaning
High≤ 1.5 km≤ 3 km, consistent basinStrong screening-level network match.
Medium≤ 5 km≤ 8 kmPlausible match; inspect source geometry for high-stakes use.
Review≤ 15 km8–20 km, catchment-supportedNetwork gap or representative-coordinate uncertainty may be material.
Unresolved> 15 km / noneno defensible connectionNo automated reach match under these rules.

Links where lake and project fall on the same reach are also marked Review, because a generalized reach cannot prove their order within it.

7. Screening scores

All scores are transparent, analyst-designed prioritization indices. They are not calibrated probabilities.

PDGLs Only — link score (0–95)

ComponentMaximumRule
ICIMOD hazard rank50Rank I = 50; II = 36; III = 22; unranked = 15.
Network distance3535 × exp(−distance_km / 125); no hard cut-off.
GLO expansion evidence1010 for significant positive expansion of a High/Medium-matched lake; 5 for positive but not significant; otherwise 0.

All GLOs — lake hazard proxy (0–100)

ComponentMaximumRule
Lake size3535 × log10(area / 0.01 km²) / 2, clamped: 0.01 km² → 0, 0.1 km² → 17.5, ≥ 1 km² → 35.
2017–2024 change25Significant positive expansion: 15 + 10 × its percentile among all significantly expanding GLO lakes. Positive but not significant: 6. Stable or shrinking: 0.
Glacier-fed connectivity1010 when GLO classifies the lake as glacier-fed; 0 otherwise.
ICIMOD expert classification30PDGL Rank I = 30; II = 20; III = 12; unranked PDGL = 8; not a PDGL = 0.
All-GLO link score = 0.6 × lake hazard proxy + 35 × exp(−distance_km / 125) (maximum 95)

Project scores (both modes)

A project's GLOF exposure screening score is its strongest link in the current mode plus a multiple-lake modifier (0 for one link, 2 for two, 3.5 for three, 5 for four or more), capped at 100. Classes: Low < 35, Moderate 35–54.9, High 55–74.9, Very High ≥ 75.

Screening priority = 80% × exposure score + 20% × log-scaled MW materiality

MW is a materiality proxy only; it is not project value, loan exposure or a loss estimate. National statistics (lakes analysed, linked lakes, connected projects and capacity) are computed separately for each mode.

8. Reading the hydrological network overlay

When a project or lake is selected, Network overlay draws the relevant part of the river network around it — not every tributary, only reaches that connect the selection to mapped lakes and projects.

Map symbols: hydropower projects are circles sized by MW and coloured by exposure class; GLO lakes are blue diamonds; ICIMOD PDGLs are magenta diamonds (darker and larger for Rank I).

9. Hydropower project data

Projects come from an administrator-maintained Google Sheet (survey, generation and operation licences), read through its public CSV export. The administrator refreshes it on demand; a refresh never re-processes the GIS sources.

10. What the current data cannot establish

11. How to use the result responsibly

Use this tool to screen, compare and prioritize further investigation. For project-level decisions, review the mapped route, snap distances, connection confidence, actual infrastructure coordinates, terrain and project protection/design information, and commission hydraulic modelling where warranted. Compare both modes: PDGLs Only reflects expert-classified hazard; All GLOs reveals exposure to lakes that have not been expert-assessed.

Do not interpret 74/100 as “74% risk.”

The number is a transparent screening index constructed from the rules above. It does not represent the probability of a GLOF, of damage, or an expected loss.