Abstract

One of the best preconditions for the sufficient monitoring of peat bog ecosystems is the collection, processing, and analysis of unique spatial data to understand peat bog dynamics. Over two seasons, we sampled groundwater level (GWL) and soil moisture (SM) ground truth data at two diverse locations at the Rokytka Peat bog within the Sumava Mountains, Czechia. These data served as reference data and were modeled with a suite of potential variables derived from digital surface models (DSMs) and RGB, multispectral, and thermal orthoimages reflecting topomorphometry, vegetation, and surface temperature information generated from drone mapping. We used 34 predictors to feed the random forest (RF) algorithm. The predictor selection, hyperparameter tuning, and performance assessment were performed with the target-oriented leave-location-out (LLO) spatial cross-validation (CV) strategy combined with forward feature selection (FFS) to avoid overfitting and to predict on unknown locations. The spatial CV performance statistics showed low (R2 = 0.12) to high (R2 = 0.78) model predictions. The predictor importance was used for model interpretation, where temperature had strong impact on GWL and SM, and we found significant contributions of other predictors, such as Normalized Difference Vegetation Index (NDVI), Normalized Difference Index (NDI), Enhanced Red-Green-Blue Vegetation Index (ERGBVE), Shape Index (SHP), Green Leaf Index (GLI), Brightness Index (BI), Coloration Index (CI), Redness Index (RI), Primary Colours Hue Index (HI), Overall Hue Index (HUE), SAGA Wetness Index (TWI), Plan Curvature (PlnCurv), Topographic Position Index (TPI), and Vector Ruggedness Measure (VRM). Additionally, we estimated the area of applicability (AOA) by presenting maps where the prediction model yielded high-quality results and where predictions were highly uncertain because machine learning (ML) models make predictions far beyond sampling locations without sampling data with no knowledge about these environments. The AOA method is well suited and unique for planning and decision-making about the best sampling strategy, most notably with limited data.

Highlights

  • We tested how well the peat bog groundwater level (GWL) and soil moisture (SM) can be predicted using multi-source and multitemporal ultrahigh-resolution UAV maps with leave-location-out (LLO) cross-validation (CV) prediction models based on random forest (RF) machine learning (ML) algorithm

  • We selected temperature soil information based on thermal data to explore the thermal potential on GWL and SM and topomorphometric variables (Slope, ProfCurv, PlnCurvc, WEI, TRI, Vector Ruggedness Measure (VRM), Topographic Position Index (TPI), and TWI) derived from digital surface models (DSMs) to investigate microtopomorphometric controls on GWL and SM patterns

  • Predictions of the variable importance have proven the dominant impact of temperature on GWL and SM and extremely significant contributions of other predictors, such as Normalized Difference Vegetation Index (NDVI), Normalized Difference Index (NDI), Enhanced Red-Green-Blue Vegetation Index (ERGBVE), Shape Index (SHP), Green Leaf Index (GLI), Brightness Index (BI), Coloration Index (CI), Redness Index (RI), Hue Index (HI), TWI, Plan Curvature (PlnCurv), TPI, and VRM1

Read more

Summary

Introduction

Peatlands as a group of wetlands are essential for the landscape and environment because they provide a wide range of critical ecosystem services [1], water-quality improvement, flood abatement, and habitat functions. Peatlands are decreasing globally in terms of their condition and diversity through habitat loss, climate change, and pollution [2]. A subdivision of peatlands, in particular, are significant water-logged reservoirs with a specific hydrological regime [3], representing habitats dominated by sphagnum moss, stored organic matter, a high water table, and low pH [4,5]. The Sumava Mountains (Sumava Mts., Bohemian Forest) feature the most extensive peat bog complex in Central Europe due to their specific geology and morphology [6]

Objectives
Methods
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call