scholarly journals Reducing the uncertainty of parameters controlling seasonal carbon and water fluxes in Chinese forests and its implication for simulated climate sensitivities

2017 ◽  
Vol 31 (8) ◽  
pp. 1344-1366 ◽  
Author(s):  
Yue Li ◽  
Hui Yang ◽  
Tao Wang ◽  
Natasha MacBean ◽  
Cédric Bacour ◽  
...  
Keyword(s):  
Water Fluxes ◽  
Simulated Climate ◽  
Uncertainty Of Parameters

Emissions of porewater compounds and gases from the subaquatic sediment disposal site “rodewischhafen”, hamburg harbour

1998 ◽  
Vol 37 (6-7) ◽  
pp. 87-93 ◽  
Author(s):  
M. Kussmaul ◽  
A. Groengroeft ◽  
H. Koethe
Keyword(s):  
Water Surface ◽  
Disposal Site ◽  
Dredged Material ◽  
Water Fluxes ◽  
Gas Emissions ◽  
Fine Grained ◽  
Deposit Surface ◽  
Groundwater Samples ◽  
High Concentrations ◽  
Mud Deposit

In the year 1993 a confined and unused harbour basin was used to store 290,000 m3 of fine-grained dredged material from Hamburg harbour. About 70% of the deposit surface was water covered. The edge areas were above the water table and covered with reed. Emissions of dissolved compounds into the groundwater, as well as surface gas emissions were measured from 1994 to 1996. As indicators for water fluxes from the deposit we used NH4+ and HCO3− because of their high concentrations in mud porewater in comparison to groundwater. The average concentrations of NH4+ and HCO3− in the porewater increased during 2 years from 85 to 250 mg NH4+ 1−1 and from 2.0 to 3.1 g HCO3− 1−1, while the groundwater samples showed constant values of 8 mg NH4+ 1−1 and 0.7 g HCO3− 1−1. Furthermore, the average gas emissions over the water surface were 3.2 g CH4 m−2 d−1 and 0.8 g CO2 m−2 d−1. In contrast, no methane and 3.0 g CO2 m−2 d−1 were emitted from land areas. The results indicated, that there were no significant emissions of mud porewater compounds into the groundwater but high CH4-emissions over the water covered surface of the mud deposit.

scholarly journals Growth Responses of Boreal Scots Pine, Norway Spruce and Silver Birch Seedlings to Simulated Climate Warming over Three Growing Seasons in a Controlled Field Experiment

Forests ◽  
2020 ◽  
Vol 11 (9) ◽  
pp. 943
Author(s):  
Katri Nissinen ◽  
Virpi Virjamo ◽  
Antti Kilpeläinen ◽  
Veli-Pekka Ikonen ◽  
Laura Pikkarainen ◽  
...  
Keyword(s):  
Norway Spruce ◽  
Scots Pine ◽  
Root Biomass ◽  
Growing Season ◽  
Silver Birch ◽  
Shoot Biomass ◽  
Growth Responses ◽  
Growing Seasons ◽  
Simulated Climate ◽  
Shoot And Root Biomass

We studied the growth responses of boreal Scots pine (Pinus sylvestris L.), Norway spruce (Picea abies L. Karst.) and silver birch (Betula pendula Roth) seedlings to simulated climate warming of an average of 1.3 °C over the growing season in a controlled field experiment in central Finland. We had six replicate plots for elevated and ambient temperature for each tree species. The warming treatment lasted for the conifers for three growing seasons and for the birch two growing seasons. We measured the height and diameter growth of all the seedlings weekly during the growing season. The shoot and root biomass and their ratios were measured annually in one-third of seedlings harvested from each plot in autumn. After two growing seasons, the height, diameter and shoot biomass were 45%, 19% and 41% larger in silver birch seedlings under the warming treatment, but the root biomass was clearly less affected. After three growing seasons, the height, diameter, shoot and root biomass were under a warming treatment 39, 47, 189 and 113% greater in Scots pine, but the root:shoot ratio 29% lower, respectively. The corresponding responses of Norway spruce to warming were clearly smaller (e.g., shoot biomass 46% higher under a warming treatment). As a comparison, the relative response of height growth in silver birch was after two growing seasons equal to that measured in Scots pine after three growing seasons. Based on our findings, especially silver birch seedlings, but also Scots pine seedlings benefitted from warming, which should be taken into account in forest regeneration in the future.

scholarly journals Comparison of blue and green water fluxes for different land use classes in a semi-arid cultivated catchment using remote sensing

2021 ◽  
Vol 36 ◽  
pp. 100860
Author(s):  
Anna Msigwa ◽  
Hans C. Komakech ◽  
Elga Salvadore ◽  
Solomon Seyoum ◽  
Marloes L. Mul ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Land Use ◽  
Green Water ◽  
Water Fluxes ◽  
Semi Arid

scholarly journals Effect of Salinity on Evaporation from Water Surface in Bench-Scale Testing

Water ◽  
2021 ◽  
Vol 13 (15) ◽  
pp. 2067
Author(s):  
Jared Suchan ◽  
Shahid Azam
Keyword(s):  
Small Variation ◽  
Arid Environments ◽  
Test Results ◽  
Canadian Prairies ◽  
Theoretical Contribution ◽  
Bench Scale ◽  
Data Scatter ◽  
Simulated Climate ◽  
Evaporative Flux ◽  
Simulator Test

Freshwater and hypersaline lakes in arid and semi-arid environments are crucial from agricultural, industrial, and ecological perspectives. The purpose of this paper was to investigate the effect of salinity on evaporation from water surfaces. The main achievement of this research is the successful capture of simulated climate–surface interactions prevalent in the Canadian Prairies using a custom-built bench-scale atmospheric simulator. Test results indicated that the evaporative flux has a large variation during spring (water/brine: 1452/764 10−4 g·s−1·m−2 and 613/230 × 10−4 g·s−1·m−2 night) and summer (1856/1187 × 10−4 g·s−1·m−2 day and 1059/394 × 10−4g·s−1·m−2 night), and small variation in the fall (1591/915 × 10−4 g·s−1·m−2 and 1790/1048 × 10−4 g·s−1·m−2 night). The primary theoretical contribution of this research is that the evaporation rate from distilled water is twice that of saturated brine. The measured data for water correlated well with mathematical estimates; data scatter was evenly distributed and within one standard deviation of the equality line, whereas the brine data mostly plotted above the equality line. The newly developed 2:1 water–brine correlation for evaporation was found to follow the combination equations with the Monteith model best matching the measurements.

scholarly journals Glaciation and deglaciation mechanisms in a coupled two-dimensional climate—ice-sheet model

1993 ◽  
Vol 39 (131) ◽  
pp. 45-49 ◽  
Author(s):  
André Berger ◽  
Hubert Gallée ◽  
Christian Tricot
Keyword(s):  
Ice Core ◽  
Ice Sheets ◽  
Low Frequency ◽  
Two Dimensional ◽  
Atmospheric Concentration ◽  
Last Glacial ◽  
Simulated Climate ◽  
Milankovitch Theory ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Abstract A two-dimensional model which links the atmosphere, the mixed layer of the ocean, the sea ice, the continents, the ice sheets and their underlying bedrock has been used to test the Milankovitch theory over the last glacial—interglacial cycle. It was found that the orbital variations alone can induce, in such a system, feed-backs sufficient to generate the low-frequency part of the climatic variations over the last 122 kyear. These simulated variations at the astronomical time-scale are broadly in agreement with ice volume and sea-level reconstructions independently obtained from geological data. Imperfections in the simulated climate were the insufficient southward extent of the ice sheets and the too small hemispheric cooling during the last glacial maximum. These deficiencies were partly remedied in a further experiment (Gallée and others, in press) by using the time-dependent CO2 atmospheric concentration given by the Vostok ice core in addition to the astronomical forcing. For this second experiment, the main mechanisms and feedbacks responsible for the glaciation and the deglaciation in the model are discussed here.

Effects of fine-scale soil moisture and canopy heterogeneity on energy and water fluxes in a northern temperate mixed forest

2014 ◽  
Vol 184 ◽  
pp. 243-256 ◽  
Author(s):  
Lingli He ◽  
Valeriy Y. Ivanov ◽  
Gil Bohrer ◽  
Kyle D. Maurer ◽  
Christoph S. Vogel ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Mixed Forest ◽  
Fine Scale ◽  
Water Fluxes ◽  
Temperate Mixed Forest

scholarly journals The effect of plant water storage on water fluxes within the coupled soil-plant system

2016 ◽  
Vol 213 (3) ◽  
pp. 1093-1106 ◽  
Author(s):  
Cheng-Wei Huang ◽  
Jean-Christophe Domec ◽  
Eric J. Ward ◽  
Tomer Duman ◽  
Gabriele Manoli ◽  
...  
Keyword(s):  
Water Storage ◽  
Plant Water ◽  
Water Fluxes ◽  
Plant System
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