River Info
Exploration Summary: Lobu
Lobu is a major watercourse system located in Papua New Guinea at coordinates 5.2891° S, 151.1184° E. Symphony of Horizon estimates a main-stem length of 33.03 km and a drainage basin area of 159 km² from its hydrological network database. The river system reaches Strahler stream order 4 and connects an extensive network of tributaries across its catchment area. This profile combines river-network geometry, basin characteristics, hydrological modeling, geomorphometric measurements, elevation analysis, and environmental indicators to provide a comprehensive scientific overview of the Lobu system.
Frequently Asked Questions About Lobu
Lobu is located in Papua New Guinea. Geographically, it lies approximately at coordinates 5.2891° S, 151.1184° E. You can inspect its spatial position and geographic boundaries on the interactive map above.
Lobu features a main stem length of 33.03 km and drains a watershed covering 159 km². It operates with a Strahler stream order of 4.
Lobu was formed through regional geomorphological processes, shaped by long-term weathering, lithological structures, and tectonic movement.
Yes, Lobu can be explored. You can find nearby routes, natural discovery points, and regional markers under the "Nearby Discovery" tab. Visitors should check local environmental regulations and travel advisories before planning a visit.
| Main Stem | 33.03 km |
| Total System | 109.94 km |
| Basin Area | 159 km² |
| Order | 4 |
| River Order | 4 |
| Drainage Area | 159 km² |
| Main Stem | 33.03 km |
| Total Length | 109.94 km |
Geological Profile
Lithology & Rock Formation
This location is primarily characterized by Basic Volcanic Rocks formations.
Scientific Note:Geological data is sourced from the Global Lithological Map (GLiM). Formation types influence local soil chemistry, water pH, and ecological biodiversity.
Hydrological network complexity, bifurcation dynamics and drainage patterns
An index of how finely carved the basin is. A **Medium** texture indicates a **balanced erosion pattern**.
The Elongation Ratio of **0.431** indicates that this catchment is **highly elongated, which slows down flood propagation and peak flow times**.
An average Bifurcation Ratio ($R_b$) of **2.92** suggests a **highly structural-fault-driven layout with elevated peak run-offs**.
Contributes 100% of total flow
Glacier Share: 0% from 0.0 km² area
Max monthly average runoff rate
This river system is primarily fed by seasonal precipitation, driving warm and nutrient-dense aquatic environments.
This river system drains and interacts directly with the **West New Britain Basin** catchment. Environmental factors, soil composition, and precipitation patterns within this basin directly determine the river's flow dynamics and water budget.
The water budget of this river segment is modeled using a dual-input empirical hydrological algorithm:
- Rainwater Runoff: Estimated via localized precipitation depth, calibrated by spatial intersection with high-resolution global basins.✓ Hydration successful: Intersected with real localized precipitation datasets.
- Glacier Meltwater: Tracks upstream glaciers within a 10 km spatial buffer of the headwater network. Glacier ablation is modeled at a baseline rate of 2.5m/year ice-equivalent depth, distributed monthly based on seasonal solar elevation in the hemisphere.
- Assumptions: Calculations use a dynamic, basin-specific runoff coefficient ($C_{\text{dynamic}} = 0.872, meaning 87.2% of precipitation is converted to river flow). This dynamic factor is calculated as the ratio of local annual runoff to precipitation ($R/P$) from HydroSHEDS basin data to resolve local evapotranspiration and soil permeability factors.
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