Restoration of natural secondary forests and afforestation of introduced tree species are major effective measures for revegetation. The semi-arid Loess Plateau region, characterized by fragile ecosystems and severe soil erosion, is a key area for ecological restoration and protection in China. To illustrate water use characteristics and adaptation to drought in the main forests in this area, we monitored the xylem sap flow of two typical forest communities, a secondary natural forest dominated by oak ( Quercus liaotungensis) and a pure plantation of black locust ( Robinia pseudoacacia), during 2011‒2019 using Granier-type thermal dissipation probes. Solar radiation, air temperature, relative humidity, precipitation, and soil water content were measured simultaneously. Throughout the whole study period, the mean diameter at breast height and total sapwood area increased by 4.5 cm and 1.10 m 2 ha -1 in the oak forest and by 1.0 cm and 0.22 m 2 ha -1, respectively, in the black locust plantation. The monthly stand transpiration was jointly determined by phenological and meteorological factors. At the annual timescale, transpiration of the oak stand was significantly correlated with potential evapotranspiration and rainfall in the previous year, whereas a significant positive relationship was detected between stand transpiration and soil water content in the black locust stand. The analyses of differences between dry and wet years showed that, the oak forest exhibited significantly different parameters in the regression analysis of stand transpiration to vapor pressure deficit. While only one parameter was clearly distinct in the black locust plantation, suggesting that its transpiration status did not fully recover even in wet years. The management of black locust plantations with weakened growth conditions should be adjusted under prolonged drought conditions. In contrast, oak forest can maintain the water balance and stable growth by efficiently controlling stomatal behavior.

Changes in water and nitrogen availability can affect the structure and function of arid ecosystems. How these resources affect aboveground primary productivity (ANPP) remains far from clear. We examined the N and water limitation of ANPP from the species to the community level and the response of ANPP to annual precipitation in a Patagonian steppe. We conducted a 7-year field experiment with water addition (+W), nitrogen addition (+N), and +NW. Destructive methods for grasses and allometric relationships for shrubs were used to assess ANPP and vegetation indices (NDVI and MSAVI2) to estimate community ANPP. An increase in ANPP of one grass species ( Papposstipa humilis) and a decrease of the grass Poa ligularis under +N were observed. Some shrubs species exhibited mortality under nitrogen addition. Nitrogen exerted a positive effect on grass ANPP and amplified the sensitivity of grass ANPP to annual precipitation. However, +N had not effects on the shrub ANPP and shrub ANPP-precipitation relationship. Water addition by itself had no effect on ANPP for either shrubs or grasses. However, shrubs responded positively to an unusually wet year regardless of treatment and were also more sensitive to changes in annual precipitation than grasses. Total ANPP increased significantly in +N relative to the C and +W, but without changes in the sensitivity to annual precipitation. The results suggest that the responses of grasses and shrubs to water inputs is driven by soil moisture redistribution and rooting depth and that grass and community ANPP is more limited by N than by water.

Analyzing the dynamics of landscape connectivity is of great significance for biodiversity conservation, but the description of multiple ecological processes and the depth of coupling requires to be strengthen. Taking the grassland of Poyang Lake as a case, based on the integrated perspective of habitat and biology, comprehensively considering the ecological process of water level change and species diffusion, this study firstly analyzed the changes of landscape connectivity of grassland with different water levels and diffusion distances by using the graph-based connectivity indices. then, landscape pattern indices were applied to analyze the dynamics of landscape pattern of grassland and further study the effects of landscape pattern on connectivity. The results showed as follows: (1) From the perspective of habitat, grassland connectivity showed a sharp decrease with the increase of water level. From the perspective of ecology, the species diffusion distance had an absolutely positive impact on landscape connectivity. With the increase of diffusion distance, grassland connectivity increased significantly. (2) The dynamics of landscape pattern of grassland showed that with the increase of water level, the patch area shrank, the patch shape tended to be simple, the patch density decreased and the patch fragmentation aggravated. (3) The correlation results between landscape pattern and connectivity indicated that F had a significant positive relationship with PD, ED, PC had a strong significant positive relationship with LPI, COHESION, and NC had a negative relationship with LPI, ED, COHESION. This study provides theoretical guidance for the conservation and management of grassland in Poyang Lake.

1. The flow regime of a river is well established as being one of the key drivers of riverine ecosystem type, diversity and condition. This is especially true of seasonal rivers that experience a cease to flow period over the dry months of the year. 2. In order to effectively assess changes to the flow regime, it is required that flow data be quantified into metrics for ease of assessment and to effectively relate changes to environmental outcomes. 3. Previous methods have used large numbers of, often complex, flow metrics to assess the flow regime. These metrics are often highly internally correlated with each other which may pose problems when considering how these metrics are assessed. The metrics are also often complicated which introduces issues for communication of results. We suggest that due to high internal correlation between metrics, significantly fewer metrics are required to describe the flow regime, and owing to the high correlation within same season flow metrics, simple metrics can be selected. 4. We report on a series of six flow metrics that cover the whole of the flow regime, that are reported annually and that are simple to assess and interpret. We then apply those six metrics to establish environmental water requirements for the North Para River in the Barossa Valley of South Australia. 5. Environmental water requirements are defined using upper and lower bounds of a moving average for each metric, rather than a defined threshold. We suggest this better reflects the highly variable nature of seasonal rivers, and the subsequent tolerances of the flora and fauna that inhabit them.

The spatiotemporal variability of groundwater level (GWL) is an important property of peatland hydrology that directly affects fluctuations of water storage. Nonetheless, current understanding of the variations of GWL in different time scales still remains unclear. In this study, two peatland watersheds (0.151 km 2 for W1 and 0.844 km 2 for W2) in the Zoige Basin in the Source Region of the Yellow River (SRYR) were selected for monitoring the temporal variability of GWL using self-recorded water loggers during 2017-2021. The main results demonstrate that: (1) GWL variations tended to be controlled by gully drainage in sites adjacent to the gully and be more synchronized with rainfall in sites distant from the gully. The GWL near the gully that cuts through the peat layer was lower than that near the gully without cutting through the peat layer, with a maximum difference between the former and the latter of 58.3 cm, indicating the effect of longitudinal attenuation of the GWL in W1. (2) Because rainfall had a lag effect on the GWL, the length of lag gradually decreased with increased rainfall intensity (i.e., the lag time of sites far away from the gully was about 18 min shorter than that of sites close to the gully in W1). (3) The peak values of the GWL occurred simultaneously with the maximum and minimum rainfall in W2, and the peak occurrence time was related to the ratio of precipitation to evaporation. In the downstream sites, GWL fluctuated more intensively than the upstream ones in W2. Moreover, the average GWL of the upstream sites was 14.3 cm higher than that of the middle ones, indicating a decreasing trend of water storage along the gully. (4) The GWL discrepancy between wet and dry seasons was explicit, but the difference was smaller in the upstream sites due to limited gully incision and higher water storage within the peat layer. Additionally, rainy days dominate the GWL change in wet and dry seasons, but the different rainfall intensity resulted in a stable GWL in the dry season and an oscillating GWL in the wet season in W2. This study uncovers the spatio-temporal variation of groundwater level in two peatland watersheds, which is of great significance for understanding runoff variation, ecohydrological processes, and wetland shrinkage in the SRYR.

The ecological restoration projects (ERPs) sig[1](#fn-0002)nificantly affect the water conservation function (WCF) of the Taihang Mountain area. However, a comprehensive understanding of the ecological effects of water conservation (WC) in different ecological engineering (EE) areas still needs to be improved, which limits the optimization and implementation of ERPs in semi-arid climate areas. In this study, we employed the integrated valuation of ecosystem services and trade-offs (InVEST) model to evaluate the differences in WCF among different ERPs in the Taihang Mountain area. Additionally, we used the structural equation model (SEM) to explore the influence of various factors on WCF, including EE factors. The results showed the following: (1) The total amount of WC in the Taihang Mountain area increased yearly from 2000 to 2020, with an 85.25% increase in 21 years. The WCF showed a trend of transferring to a higher level. (2) The forest recovery (FR) project showed the highest average WC, followed by the grassland recovery (GR) project. FR and GR together provided 61.12% of the WC amount in the EE area. The cropland recovery (CR) project increased the WC by 22.85% compared with the non-ecological engineering area. The WC capacity of the 21-year artificial forest could only reach 70.92% of the natural forest. FR was found to be the most potential ecological restoration type, while CR and GR were the most effective. (3) The enhancement of WCP in the study area resulted from multiple factors. The composite variable SEM revealed four main factors affecting WC (R 2 = 0.427), ranked as follows: climate change > site conditions > EE > society-economy (0.390 > 0.247 > 0.177 > 0.043), of which the EE factor accounted for 20.65%. Precipitation and root depth were the most critical factors affecting WCP, according to the random forest model. (4) The impact of EE on WC varied with altitude, and the effect of the hilly zone was 1.5 times that of the sub-alpine zone. Therefore, the WC effect of ERPs is different due to different types and regions. EE measures should be optimized according to the actual situation to cope with the uncertainty of WC caused by probable extreme climate in the future. Overall, our study provides scientific support for evaluating the impact of ERPs on WCF in semi-arid areas of China.

A document by Hannah A. Varani. Click on the document to view its contents.

Water transport timescales (WTTs) quantify how long it takes for water to travel through or remain in a system and are often cast as indicators of ecosystem function and health. Such timescales are known to be affected by vegetation in various environments. We quantify the impact of floodplain vegetation on WTTs within the Wax Lake Delta (WLD), a river delta system in Louisiana, USA, using a high-resolution Delft3D Flexible Mesh (DFM) model incorporating vegetation-induced flow resistance. We show that increased vegetation density leads to extended WTTs within vegetated sections of WLD while fostering flow localization and accelerating transport within distributary channels. We find that the presence or absence of floodplain vegetation significantly influences the volumetric flow directed toward the floodplain, with spatial distribution exerting more control than vegetation density. Vegetation density and spatial arrangement have minimal impact on flow directed out of the deltaic floodplain, indicating that vegetation does not constrain flow across the bayward boundary. Floodplain vegetation strongly influences local-scale transport timescales within the deltaic floodplain but minimally affects water age distributions within distributary channels. Furthermore, network-scale water age distribution remains largely unaffected by vegetation density and spatial arrangement, except for slight modifications in the heavy right tail of the distribution. These findings contribute to a better understanding of how vegetation affects deltaic hydrology across scales, highlighting the importance of considering multi-scale vegetation influences for coastal restoration and management strategies.

Terrestrial water energy coupling (WEC), in the form of the non-linear relationship between Soil Moisture (SM) and evaporative fraction (EF, ratio of actual and potential evapotranspiration), controls critical ecohydrological processes. We investigate and parameterize the evolution of global SM–EF coupling from the field to remote-sensing (RS)-footprint. The field-scale EF and SM were obtained from 163 eddy covariance (EC) and SM sensors at various network (Texas Water Observatory and FLUXNET) sites around the globe. Remote-sensing (RS)-scale EF and SM estimates were obtained from Moderate-resolution Imaging Spectroradiometer (MODIS) and Soil Moisture Active Passive (SMAP) sensors, respectively. We estimate the effective thresholds of the WEC regimes from both EC and satellite datasets to highlight the influence of subgrid-scale heterogeneity, scaling, and observational constraints on the evolution of WEC regimes from field to RS-footprint scale. We compare the critical WEC thresholds of the water- and energy-limited regimes with an SM drydown-based approach and highlight the similarities between both methods in partitioning dominant WEC regimes. EF and SM are strongly coupled in dryland arid and semi-arid regions compared to humid climates. WEC regimes and thresholds have strong interseason variability due to dynamic interactions between soil, vegetation, and atmosphere at the RS-footprint scale. In contrast, field-scale SM-EF coupling is influenced predominantly by agricultural /land-use practices and soil conditions. Hence, future development of Earth-System/Land-Surface models must account for the inter-scale differences in the coupling between terrestrial water and energy fluxes representative of the “ effective” processes at large spatial scales.

The dominant plant species in many African wetlands is Cyperus papyrus. Its adaption to saturated and low oxygen conditions and its dense structure and height provide breeding and feeding grounds for unique flora and fauna. As a keystone species adapted to local hydrology, the flow regime of papyrus offers the full range of hydrologic conditions and events essential to ecosystem health. However, no study has attempted to link papyrus wetlands’ flow regimes to their biologically-relevant hydrologic attributes. The Indicators of Hydrologic Alteration (IHA) enable the evaluation of changes to flow regimes by examining hydrologic records and linking them to biologically-relevant hydrologic characteristics through the Environmental Flow Components (EFCs) approach. This study assesses hydrologic alterations of a papyrus wetland’s flow regime due to rice irrigation. We develop a conceptual ecological model linking papyrus to hydrologic attributes to determine the consequences of changed EFCs (extreme low flows, base flow, high flow pulses, and small and large floods) on papyrus as a habitat. We find that agricultural water management considerably alters the magnitude, duration, timing and rate of change of EFCs for the irrigated area to catchment area ratio greater than 1:153, affecting both sexual and asexual reproduction in papyri plants. Overall, a better understanding of the threats of water diversion for agriculture is made by linking papyrus’ flow regimes to biologically-relevant hydrologic attributes. Knowledge of the roles of the various EFCs could provide opportunities for conserving and protecting papyrus wetlands, especially for systems at risk of altered flows.

Extraordinary events are rarely observable in a single rainfall gauge, and this make extremely challenging the correct prediction of their arrivals. However, it may be possible to develop a more robust approach by employing a space-time modelling scheme that is able to capture the spatial dynamics of such phenomena. Therefore, a space-time Poisson model of rainfall cells with circular shape and random depth has been exploited for the first time to interpret the behaviour of this family of extraordinary events. This category of events that may be connected to larger meteorological phenomena not necessarily connected with local heterogeneity of the landscape. Following the identification of the observed extraordinary event across southern Italy, six zones with significantly different dynamics in terms of the frequency of such extremes were identified. Subsequently, a simple mathematical representation was adopted to calibrate the model parameters, leading to an estimate of regional probability distributions defined on the space-time occurrences of extraordinary events over homogeneous zones. The approach allows to overcome the limitations posed by point observations allowed the definition of a probability distribution that pertains to an entire area rather than just a point. The obtained quantiles of rainfall estimated seems to align well with the upper bound of the probability distribution of the annual maxima observed over the areas of interests.

Hydropeaking (the release of water pulses at hydropower plants) results in temporary reductions in river channel water-covered area downstream, which may cause fish mortality through stranding. We used a mechanistic modelling approach to examine how, both, the form of the hydropeaking cycle, and the characteristics of the affected fish, control how hydropeaking may cause stranding mortality of fish. We modelled the response of Atlantic parr to hydropeaking in a regulated watercourse in central Norway (the River Nidelva) using an individual-based population model designed explicitly to examine fish behavior and stranding mortality during hydropeaking. A response to hydropeaking, involving migration from the river banks toward the mid-channel on down-ramping, and a return to the river banks on up-ramping, was based on individuals being parameterized to migrate to habitat properties that spatially changed throughout the hydropeaking cycle. We found that stranding mortality was strongly dependent on both the form of the hydropeaking cycle and on the fish response. Total stranding mortality was more dependent on the down-ramping speed than the duration of the minimum flow period. Total stranding mortality was greatest when there was a low movement speed, leading to individuals being stranded, combined with a high probability of dying per unit of time when stranded. Given the sensitivity of mortality to the fish response, and the lack of detailed field studies quantifying this, we conclude that this area requires further controlled studies for parameterizing models used to predict effects of hydropeaking on fish.

1. Opisthorchis viverrini is a water-based disease-causing parasite whose public health implications are relevant in particular in Southeast Asia despite broad control efforts and education campaigns. Untreated or chronic infections often lead to severe hepatobiliary morbidity including cholangiocarcinoma, an often lethal bile duct cancer. The liver fluke O. viverrini is the causative agent of opisthorchiasis, and can be contracted by consumption of raw fish, after which it settles in the small intrahepatic bile ducts. The life cycle involves, besides freshwater snails in which asexual reproduction takes place, freshwater cyprinid fishes (family Cyprinidae) as intermediate hosts. Piscivorous mammals, including humans, dogs and cats, act as definitive hosts. 2. Here, we propose a spatially explicit model for the transmission dynamics in realistic freshwater environments. Our model generalizes existing mathematical models, in particular by assimilating novel types of spreading mechanisms in space and time. We explore theoretically the range of outcomes that the proposed framework produces, and its basic sensitivity and stability analyses; 3. Our study emphasizes that hydrological connectivity is key to shaping patterns of disease spread. Fish distribution and mobility also affect disease inroads. Our study provides baseline information on the role of connected freshwater bodies and their suitability for intermediate and final hosts. The distributions of fish catch and fish market supplies are also considered because they affect the spatiotemporal spread of opisthorchiasis; 4. Adding a spatial resolution to transmission models changes fundamentally the epidemiological descriptions and the related scenarios of disease propagation and allows an improved description of the ecology of hosts, parasites, and their infection cycles. 5. The improvement that the work provides is a much more realistic description of the environment where infection cycles develop and spread, reflected in the inclusion of relevant, hitherto neglected, epidemiological factors.

Coastal dunes are the highest natural features on a barrier island, where they protect beach communities,infrastructure, and low-energy back-barrier ecosystems from flooding and erosion during storms and otherhigh-water events. Their formation, and post-storm recovery, is a result of a subtle competition betweenthe physical and biological processes controlling the initial stages of dune growth. Vegetation colonizes abarren back-beach and traps wind-driven (aeolian) sand to form dunes, but at low enough elevation plantscan be eroded by water-driven transport during random flooding events, which slows down or prevents duneformation. This competition has been previously investigated using both process-based and analytical models.However, the effect of finite vegetation recovery times together with the precise stochastic nature of floodingevents has not been taken into account before. A recent stochastic dune model assumed vegetation grows andrecovers instantaneously, whereas an existing process-based dune model, the Coastal Dune Model (CDM),didn’t properly resolve the stochastic flooding events. Here, we address this knowledge gap by adding amuch more realistic description of high-water events of the stochastic model to CDM and investigate therole of vegetation growth and recovery times in dune formation. We first replicate the stochastic modelpredictions assuming instantaneous vegetation growth. We then define the vegetation colonization time andrelate it to the initial dune formation time. Since dune formation requires the presence of vegetation, a finitecolonization time leads to an expected lag in dune formation and recovery. Depending on the competitionbetween vegetation growth and aeolian erosion, we find that dune dynamics can be divided into two regimes:one with a stable (static) vegetated dune and another one with a mobile, partially vegetated, dune propagatinglandward. Within the stable dune regime, the influence of vegetation on dune recovery is solely controlledby the relation between the vegetation colonization time, the dune growth time after plant colonization,and the return period of high-water events flooding the back-beach. We introduce two control parametersbased on these times and use them to describe a simplified phase space of the dune state. We then find a simple analytical expression for the transition from a ‘high’ state with mature dunes to a ‘low’ state devoid of dunes based on the competition between dune recovery time controlled by vegetation and the flooding frequency. Finally, we use the transition threshold to propose a vulnerability indicator for dune recovery as the minimum elevation after an overwash required for vegetation to recover.