scholarly journals Increase in perennial forage yields driven by climate change, at Apukka Research Station, Rovaniemi, 1980-2017

2020 ◽  
Vol 29 (2) ◽  
Author(s):  
Oiva Niemeläinen ◽  
Antti Hannukkala ◽  
Lauri Jauhiainen ◽  
Kaija Hakala ◽  
Markku Niskanen ◽  
...  
Keyword(s):  
Climate Change ◽  
Festuca Arundinacea ◽  
Ground Cover ◽  
Growing Season ◽  
Phleum Pratense ◽  
Research Station ◽  
Strong Impact ◽  
Meadow Fescue ◽  
Forage Crops ◽  
The North

The official variety trials at Rovaniemi, Finland (66.58°N, 26.01°E) in 1980–2017 show a substantial increase in dry matter yields (DMY) of timothy (Phleum pratense), meadow fescue (Festuca pratensis) and tall fescue (Festuca arundinacea), coinciding with a 156 °Cd increase in the average growing season Tsum and a 461 °Cd decrease in the average winter frost sum for the same period. The annual DMY of timothy was 3128, 4668, 8385 and 9352 kg ha-1 in the periods (P) 1980–1989 (P1), 1990–1999 (P2), 2000–2009 (P3), and 2010–2017 (P4). The first cut yielded 1792, 2166, 4008 and 4473, and the second cut 1337, 2503, 4378 and 4879 kg ha-1, respectively. Yields of meadow fescue followed a similar pattern. The first cut was about ten days and the second cut about one week earlier on P4 than on P1. Shorter snow cover period, milder winters, higher live ground cover of timothy in spring, and higher temperature sum during the growing season were most likely responsible for the yield increase. The results indicate a strong impact of climate change on DMY of perennial forage crops in the north.

Alternative turnoff strategies for Kimberley beef cattle. 1. Live animal performance and carcass characteristics.

1987 ◽  
Vol 9 (2) ◽  
pp. 61 ◽  
Author(s):  
WJ Ryan ◽  
D Pratchett ◽  
BL McIntyre
Keyword(s):  
Beef Cattle ◽  
Carcass Characteristics ◽  
Growing Season ◽  
Agricultural Area ◽  
Research Station ◽  
Food Conversion ◽  
Live Animal ◽  
Grazing Season ◽  
Growing Seasons ◽  
The North

In June 1980, 190 Kimberley Shorthorn steers from five properties in the Kimberley were divided into three age categories. Half were sent to Chapman Research Station (CRS) in the agricultural area of Western Australia and the remainder stayed at Ord Regeneration Research Station (ORRS) in the Kimberley. Animals in both locations grazed for either one or two pasture growing seasons and a third group was fed a concentrate ration based on grain after the first growing season. Cattle lost between 20-30 kg in handling and transport south which, together with the reduced initial grazing season, led to gains of only 50 kg while those in the north gained around 100 kg. In the second grazing season at both locations animals gained around 140 kg. Animals at ORRS laid down more fat than those at CRS. Animals fed on concentrate rations in the agricultural area grew significantly faster, but had poorer food conversion and were leaner compared with those fed in the Kimberley.

Impact of Climate Change on the North Sea Offshore Energy Sector

2018 ◽  
Author(s):  
Nicolas Fournier ◽  
Galina Guentchev ◽  
Justin Krijnen ◽  
Andy Saulter ◽  
Caroline Acton ◽  
...  
Keyword(s):  
Climate Change ◽  
Sea Level ◽  
North Sea ◽  
Wave Climate ◽  
Energy Industry ◽  
Strong Impact ◽  
Impact Of Climate Change ◽  
The North ◽  
Climate Indicators ◽  
The North Sea

The complex nature of the energy industry across extraction, transportation, processing, delivery and decommissioning creates significant challenges to how the sector responds, adapts and mitigates against risks posed by the changing future climate. Any disruption in this interconnected system will affect both industry and society. For example, in the summer of 2005 Hurricane Katrina and a month later Hurricane Rita had wide reaching impacts on the US offshore Oil and Gas industry which resulted in an increase in global oil prices due to loss of production and refinery shutdowns in the Gulf of Mexico. Preparing, mitigating and adapting to these climate changes is dependent upon identifying appropriate climate indicators as well as the associated critical operational thresholds and design criteria of the identified vulnerable assets. The characterization and understanding of the likely changes in these climate indicators will form the basis for adaptation plans and mitigating actions. The Met Office in collaboration with energy industry partners, under the Copernicus Clim4energy European project, has developed a Climate Change Risk Assessment tool, which allows the visualization and extraction of the most recent sea level and wave climate information to evaluate their future changes. This study illustrates the application of this tool for evaluation of the potential vulnerability of an offshore infrastructure in the North Sea. The analysis shows that for this asset there is a small increase in sea level of 0.20–0.30 m at the location of interest by 2050. However, there is a small decrease or no consistent changes projected in the future wave climate. This wave signal is small compared to the uncertainty of the wave projections and the associated inter-annual variability. Therefore, for the 2050s time horizon, at the location of interest, there is no strong impact of climate change at the annual scale on the significant wave height, the sea level and thus the associated climate change driven extreme water level. However, further analysis are required at the seasonal and monthly scales.

PERSISTENCE OF A RANGE OF GRASSES IN A CONTINENTAL CLIMATE

1999 ◽  
Vol 35 (1) ◽  
pp. 55-62 ◽  
Author(s):  
D. Wilman ◽  
K. H. Dong ◽  
Z. L. Jin
Keyword(s):  
Perennial Ryegrass ◽  
Tall Fescue ◽  
Festuca Arundinacea ◽  
Ground Cover ◽  
The Other ◽  
Meadow Fescue ◽  
The Third ◽  
Harvest Year ◽  
Hybrid Cultivar ◽  
Continental Climate

The possibility of growing grasses of higher quality than tall fescue (Festuca arundinacea) in a continental climate with cold winters, hot summers and low precipitation was investigated with and without irrigation at Taigu, Shanxi, China. Tall fescue was compared with perennial ryegrass (Lolium perenne), meadow fescue (Festuca pratensis) and a perennial ryegrass × meadow fescue hybrid cultivar in field swards, managed by cutting, during the year of sowing and in the three subsequent years. Tall fescue persisted satisfactorily throughout the experiment, even without irrigation. With irrigation, the other three grasses persisted satisfactorily to the end of the second harvest year and fairly satisfactorily to the end of the third harvest year. Without irrigation, the other three grasses had incomplete ground cover in the second harvest year and did not recover from the third winter.

scholarly journals THE KEY FEATURES OF THE CURRENT CLIMATE CHANGE IN THE REPUBLIC OF BELARUS

2020 ◽  
Vol 3 ◽  
pp. 22-41
Author(s):  
S.A. Lysenko ◽  
◽  
I.V. Buyakov ◽  
Keyword(s):  
Climate Change ◽  
Air Temperature ◽  
Heat Waves ◽  
Growing Season ◽  
Potential Evaporation ◽  
The South ◽  
The North ◽  
The Republic ◽  
Sum Of Active Temperatures

This paper investigates spatial and temporal features of the climate change in the Republic of Belarus during the period from 1960 to 2019. To accomplish this, we used data on daily average surface air temperature and applied decomposing the time series of these data with singular-spectrum analysis. We analyzed the principal components and long-term average anomalies of average annual, winter and summer air temperatures, the number of frosty days in the cold season and the number of winter days with thaws, the duration and heat supply of the growing season, as well as the frequency and intensity of heat waves. We also estimated the rates of moving the annual sum of active temperatures and the duration of the growing season from the south to the north of Belarus as a result of global warming. The ERA5 reanalysis estimates the spatial and temporal changes in the balance between annual rainfall and potential evaporation from 1980 to 2019. The average annual air temperature in 2000-2019 is shown to be exceeded the long-term average of this value by 1.8° C. The annual sum of active temperatures moves northward at an average speed of 120 km in 10 years with acceleration. Over the past 20 years, the rate of this displacement has doubled in comparison with the period 1980-2000. The length of the growing season moves from the south to the north at a speed of about 110 km per 10 years. It is shown that an increase in potential evaporation due to air warming when slightly changing annual amount of precipitation leads to aridization of the climate of Belarus emitting a reduction in the duration of the cold period with a simultaneous increase in the number of thaws does not contribute to the replenishment of water reserves during snowmelt. Additional damage to forestry and agriculture might be caused by heat waves, the frequency of which for 2000-2019 increased by a factor of 4 compared to the previous 20-year period. Additional damage to forestry and agriculture might be caused by heat waves, which frequency during last 19 years increased by a factor of 4 compared to the previous 20 years.

Dry matter production, fibre composition and plant characteristics of cool-season grasses under two harvest systems

1990 ◽  
Vol 115 (3) ◽  
pp. 321-326 ◽  
Author(s):  
H. T. K. Kunelius
Keyword(s):  
Festuca Arundinacea ◽  
Prince Edward Island ◽  
Lolium Multiflorum ◽  
Growing Season ◽  
Phleum Pratense ◽  
Cool Season ◽  
Primary Growth ◽  
Matter Production ◽  
Acid Detergent Fibre ◽  
Cutting Height

SUMMARYCultivars of Phleum pratense, Festuca pratensis, Festuca arundinacea, Dactylis glomerata and Lolium × Festuca hybrids were exposed to 4- and 3-cut harvest systems in Prince Edward Island, Canada, in 1985–87. Lolium perenne × F. pratensis, Lolium multiflorum × F. pratensis and L. multiftorum × F. arundinacea hybrids and D. glomerata had more uniform growth among the harvests than other grasses during the growing season. L. perenne × F. pratensis and L. multiflorum × F. pratensis had lower contents of neutral and acid detergent fibre than other grass cultivars, particularly early in the growing season. P. pratense cv. Farol had the lowest and L. perenne × F. pratensis cv. Prior the highest tiller population density. The stem apex of all cultivars was above the cutting height of 5 cm in c. 50% of tillers of primary growth. Leaf area per tiller was largest for P. pratense cv. Farol in the primary growth stage but differences were small in subsequent cuts.

scholarly journals ECOLOGICAL TESTING OF PERENNIAL GRASS VARIETIES DEVELOPED BY THE NORTH CAUCASIAN FEDERAL SCIENTIFIC AGRICULTURAL CENTERUNDER THE CONDITIONS OF THE REPUBLIC OF ALTAI

2021 ◽  
pp. 20-25
Author(s):  
N.V. Ledyayeva ◽  
Keyword(s):  
Dry Matter ◽  
Trifolium Pratense ◽  
Perennial Grass ◽  
Red Clover ◽  
Phleum Pratense ◽  
Grass Species ◽  
Meadow Fescue ◽  
The North ◽  
Digestible Protein ◽  
The Republic

When establishing polyspecies plant communities with the inclusion of new perennial grass species (cookshead (Onobrychis viciifolia Scop.), bastard alfalfa (Medicago×varia)and yellow alfalfa (Medicago falcata), Siberian wheatgrass (Agropyrum sibiricum) and tall wheatgrass (Agropyrum elongatum)), along with the species traditional-ly grown in the Republic of Altai (red clover (Trifolium pratense), awnless brome (Bromopsis inermis Leyss.), meadow fescue grass (Festuca pratensis)and common timothy (Phleum pratense)), the following most highly pro-ductive grass mixtures were identified: three-component -common timothy + alfalfa + clover (at the ratio 60:30:10), and timothy + awnless brome+ clover (at the ratio 40:30:30); four-component -awnless brome+ fescue grass+ cookshead + clover (at the ratio 30:30:30:10), and timo-thy + fescue grass+ cookshead + alfalfa (at the ratio 30:20:20:30) that may ensure a reliable gain of dry matter yield from the second year of life to 4.80-5.57 t ha. They make it possible to obtain high-nutritional hay when har-vested during the flowering stage with metabolizable ener-gy concentration up to 9.75-10.75 MJ in 1 kg of dry matter, and with digestible protein content up to 124.2-130.8 g in 1 fodder unit.

scholarly journals Climate change, growing season water deficit and vegetation activity along the north–south transect of eastern China from 1982 through 2006

2012 ◽  
Vol 16 (10) ◽  
pp. 3835-3850 ◽  
Author(s):  
P. Sun ◽  
Z. Yu ◽  
S. Liu ◽  
X. Wei ◽  
J. Wang ◽  
...  
Keyword(s):  
Climate Change ◽  
Water Deficit ◽  
Eastern China ◽  
Coniferous Forest ◽  
Growing Season ◽  
Future Climate Change ◽  
Vegetation Types ◽  
The North ◽  
Vegetation Activity ◽  
Energy Limitation

Abstract. Considerable work has been done to examine the relationship between environmental constraints and vegetation activities represented by the remote sensing-based normalized difference vegetation index (NDVI). However, the relationships along either environmental or vegetational gradients are rarely examined. The aim of this paper was to identify the vegetation types that are potentially susceptible to climate change through examining their interactions between vegetation activity and evaporative water deficit. We selected 12 major vegetation types along the north–south transect of eastern China (NSTEC), and tested their time trends in climate change, vegetation activity and water deficit during the period 1982–2006. The result showed significant warming trends accompanied by general precipitation decline in the majority of vegetation types. Despite that the whole transect increased atmospheric evaporative demand (ET0) during the study period, the actual evapotranspiration (ETa) showed divergent trends with ET0 in most vegetation types. Warming and water deficit exert counteracting controls on vegetation activity. Our study found insignificant greening trends in cold temperate coniferous forest (CTCF), temperate deciduous shrub (TDS), and three temperate herbaceous types including the meadow steppe (TMS), grass steppe (TGS) and grassland (TG), where warming exerted more effect on NDVI than offset by water deficit. The increasing growing season water deficit posed a limitation on the vegetation activity of temperate coniferous forest (TCF), mixed forest (TMF) and deciduous broad-leaved forest (TDBF). Differently, the growing season brownings in subtropical or tropical forests of coniferous (STCF), deciduous broad-leaved (SDBF), evergreen broad-leaved (SEBF) and subtropical grasslands (STG) were likely attributed to evaporative energy limitation. The growing season water deficit index (GWDI) has been formulated to assess ecohydrological equilibrium and thus indicating vegetation susceptibility to water deficit. The increasing GWDI trends in CTCF, TCF, TDS, TG, TGS and TMS indicated their rising susceptibility to future climate change.

The Analysis of Vegetation Phenology and Climate Change in the North-South Transect of Eastern China

2014 ◽  
Vol 1010-1012 ◽  
pp. 1230-1233 ◽  
Author(s):  
Zhi Wang ◽  
Shi Rong Liu
Keyword(s):  
Climate Change ◽  
Spatial Pattern ◽  
Meteorological Data ◽  
Eastern China ◽  
Terrestrial Ecosystems ◽  
Growing Season ◽  
Distribution Patterns ◽  
Observation Data ◽  
The North ◽  
Temperate Desert

In order to explore additional distribution patterns of global change to terrestrial ecosystems, phenology refers to seasonal biological life stages driven by environmental factors, and is considered to be a sensitive and precise indicator of climate change. Therefore, the author developed a ‘bottom-up’ method for first determining the phenological growing season at sample stations, and based on NOAA/AVVHRR, meteorological data, ground phonology observation data, vegetation category data, and so on. The author built a Logistic fitting model on cumulative frequency of NDVI to determine length of greenness period since 1982, then analyzed correlation between NDVI and precipitation, primarily revealed the dynamic mechanism of climate on vegetation. The spatial pattern of average turning green and wilting dates of the growing season correlated significantly with the spatial pattern of average temperatures in spring and winter across the north south transect of eastern China during 1982 to 2003; the growing season extended on average by 5 to 8 days . Temperate desert regions had the trend of increase of desertification.

scholarly journals Climate change, growing season water deficit and vegetation activity along the north-south transect of Eastern China from 1982 through 2006

2012 ◽  
Vol 9 (5) ◽  
pp. 6649-6688 ◽  
Author(s):  
P. Sun ◽  
Z. Yu ◽  
S. Liu ◽  
X. Wei ◽  
J. Wang ◽  
...  
Keyword(s):  
Climate Change ◽  
Water Deficit ◽  
Eastern China ◽  
Coniferous Forest ◽  
Growing Season ◽  
Future Climate Change ◽  
Severe Drought ◽  
Vegetation Types ◽  
The North ◽  
Vegetation Activity

Abstract. Considerable work has been done to examine the relationship between environmental constraints and vegetation activities represented by the remote sensing-based Normalized Difference Vegetation Index (NDVI). However, the relationships along either environmental or vegetation type gradients are rarely examined. The aim of this paper was to identify the vegetation types that are potentially susceptible to climate change through examining the interaction between vegetation activity and water deficit. We selected 12 major vegetation types along the north-south transect of Eastern China (NSTEC), examined their time trends from 1982 to 2006 with respect to climate change, vegetation activity and water deficit. The results showed that all vegetation types experienced warming during the study period, and the majority of them experienced precipitation decline. Warming and growing season water deficit exert counteracting controls on vegetation activity. Our study found insignificant greening trends in the northernmost cold temperate coniferous forest (CTCF), three temperate herbaceous types including the meadow steppe (TMS), grass steppe (TGS) and grassland (TG), where the growing season warming exerted more than offset effect on vegetation activity (phenology) than growing season water deficit. For the three temperate forest including the coniferous (TCF), mixed (TMF) and deciduous-broadleaved (TDBF), growing season water deficit was the main constraint on vegetation activity. Differently, the growing season browning in subtropical or tropical forests of coniferous (STCF), deciduous-broadleaved (SDBF) and evergreen-broadleaved (SEBF) and subtropical grasslands (STG) were likely attributed to decline in sunshine duration due to increased summer cloudiness. Poor water status in TDS, TG, TMS and severe drought in TGS have been identified by using growing season water deficit index (GWDI), suggested these ecosystems were subjected to severe progressing drought that may create greening trend reversal in future. The emerging water deficit in CTCF, TCF and SDBF suggested their rising susceptibility to future climate change.

scholarly journals Vegetation Phenological Changes in Multiple Landforms and Responses to Climate Change

2020 ◽  
Vol 9 (2) ◽  
pp. 111 ◽  
Author(s):  
Hongzhu Han ◽  
Jianjun Bai ◽  
Gao Ma ◽  
Jianwu Yan
Keyword(s):  
Climate Change ◽  
Vegetation Index ◽  
Normalized Difference Vegetation Index ◽  
Climatic Factors ◽  
Growing Season ◽  
Vegetation Phenology ◽  
The South ◽  
Response Characteristics ◽  
The North ◽  
Spatio Temporal

Vegetation phenology is highly sensitive to climate change, and the phenological responses of vegetation to climate factors vary over time and space. Research on the vegetation phenology in different climatic regimes will help clarify the key factors affecting vegetation changes. In this paper, based on a time-series reconstruction of Moderate-Resolution Imaging Spectroradiometer (MODIS) normalized difference vegetation index (NDVI) data using the Savitzky–Golay filtering method, the phenology parameters of vegetation were extracted, and the Spatio-temporal changes from 2001 to 2016 were analyzed. Moreover, the response characteristics of the vegetation phenology to climate changes, such as changes in temperature, precipitation, and sunshine hours, were discussed. The results showed that the responses of vegetation phenology to climatic factors varied within different climatic regimes and that the Spatio-temporal responses were primarily controlled by the local climatic and topographic conditions. The following were the three key findings. (1) The start of the growing season (SOS) has a regular variation with the latitude, and that in the north is later than that in the south. (2) In arid areas in the north, the SOS is mainly affected by the temperature, and the end of the growing season (EOS) is affected by precipitation, while in humid areas in the south, the SOS is mainly affected by precipitation, and the EOS is affected by the temperature. (3) Human activities play an important role in vegetation phenology changes. These findings would help predict and evaluate the stability of different ecosystems.

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