Anthropogenic activities are changing global precipitation regimes and result in many middle latitude arid and semiarid regions experiencing less precipitation and more extreme weather events. However, little is known about the response of active ingredient accumulation in the medicinal herb Plantago depressa Willd. Therefore, we carried out a greenhouse experiment in order to study effect of control (CK, normal water supply equal to 309 mm per four months), -30 (-WS) and +30% (+WS) of the control water supply on the photosynthesis (PN), C/N ratio, and plantamajoside accumulation in P. depressa. Our results showed that compared with the-WS and CK treatments, the +WS treatment significantly enhanced biomass, the C/N ratio, plantamajoside concentration, yield in shoots and roots, and PN, but declined the N concentration in shoots and roots. The plantamajoside concentration was positively correlated with PN, the soluble sugar content, and the C/N ratio, but negatively correlated with the N concentration. Our results suggested that, under experimental conditions, +WS increased the C/N ratio and promoted the plantamajoside accumulation of P. depressa., Z. Li, W. Bai, L. Zhang, L. Li., and Obsahuje bibliografii
This work aimed to evaluate if gas exchange and PSII photochemical activity in maize are affected by different irradiance levels during short-term exposure to elevated CO2. For this purpose gas exchange and chlorophyll a fluorescence were measured on maize plants grown at ambient CO2 concentration (control CO2) and exposed for 4 h to short-term treatments at 800 μmol(CO2) mol-1 (high CO2) at a photosynthetic photon flux density (PPFD) of either 1,000 μmol m-2 s-1 (control light) or 1,900 μmol m-2 s-1 (high light). At control light, high-CO2 leaves showed a significant decrease of net photosynthetic rate (PN) and a rise in the ratio of intercellular to ambient CO2 concentration (Ci/Ca) and water-use efficiency (WUE) compared to control CO2 leaves. No difference between CO2 concentrations for PSII effective photochemistry (ΦPSII), photochemical quenching (qp) and nonphotochemical quenching (NPQ) was detected. Under high light, high-CO2 leaves did not differ in PN, Ci/Ca, ΦPSII and NPQ, but showed an increase of WUE. These results suggest that at control light photosynthetic apparatus is negatively affected by high CO2 concentration in terms of carbon gain by limitations in photosynthetic dark reaction rather than in photochemistry. At high light, the elevated CO2 concentration did not promote an increase of photosynthesis and photochemistry but only an improvement of water balance due to increased WUE. and C. Arena, L. Vitale, A. Virzo de Santo.
C3 photosynthesis at high light is often modeled by assuming limitation by the maximum capacity of Rubisco carboxylation (VCmax) at low CO2 concentrations, by electron transport capacity (Jmax) at higher CO2 concentrations, and sometimes by
triose-phosphate utilization rate at the highest CO2 concentrations. Net photosynthetic rate (PN) at lower light is often modeled simply by assuming that it becomes limited by electron transport (J). However, it is known that Rubisco can become deactivated at less than saturating light, and it is possible that PN at low light could be limited by the rate of Rubisco carboxylation (VC) rather than J. This could have important consequences for responses of PN to CO2 and temperature at low light. In this work, PN responses to CO2 concentration of common bean, quinoa, and soybean leaves measured over a wide range of temperatures and PPFDs were compared with rates modeled assuming either VC or J limitation at limiting light. In all cases, observed rates of PN were better predicted by assuming limitation by VC rather than J at limiting light both below and above the current ambient CO2. One manifestation of this plant response was that the relative stimulation of PN with increasing the ambient CO2 concentration from 380 to 570 µmol mol-1 did not decrease at less than saturating PPFDs. The ratio of VC to VCmax at each lower PPFD varied linearly with the ratio of PN at low PPFD to PN at high PPFD measured at 380 µmol(CO2) mol-1 in all cases. This modification of the standard C3 biochemical model was much better at reproducing observed responses of light-limited PN to CO2 concentrations from
pre-industrial to projected future atmospheric concentrations., J. A. Bunce., and Obsahuje bibliografii
Brief review on the availability of General Circulation Models (GCMs) and Regional Circulation Models (RCMs) outputs for regional downscaling is presented (more in Melo, 2003; Melo, 2004). Four basic methods of regional climate change scenarios design (1st - Incremental (the simplest), 2nd - Analogue (historical or paleoclimatic), 3rd - Weather generator (artificial or based on real climatic statistics), 4th - GCMs (General Circulation Models) based) are discussed more in details. The additional one - a combined method, usually based on GCMs (mean annual/monthly warming and mean annual/monthly change in precipitation totals) and on historical analogue (statistical structure of daily/monthly data series, including physical plausibility among phenomena), was utilized in Slovakia. Finally some results of different climate change scenarios for Hurbanovo and possible user problems are listed and discussed. Special scenarios of exceptional weather events are also demanded by users, mainly from the Hydrology, Agriculture and Forestry sectors, very concise overview of such scenarios design is presented. and Príspevok prezentuje stručný prehľad dostupných modelov všeobecnej cirkulácie atmosféry (GCMs) ako aj metód na regionálnu interpretáciu výstupov GCMs. V zásade môžeme metódy konštrukcie scenárov klimatickej zmeny (zmien klímy) rozdeliť do 4 skupín: 1. Inkrementálne (prírastkové) scenáre; 2. Analógové scenáre; 3. Stochastický generátor počasia; 4. Dowscaling výstupov GCMs s regionálnou interpretáciou a využitím experimentálnych časových radov. Za piatu môžeme považovať metódu kombinovanú, ktorá využíva spoľahlivejšie scenáre na báze GCMs (zväčša teplotné a zrážkové) a pre zvyšné klimatické prvky sa pripravujú scenáre ako analógy korelačnou alebo regresnou metódou. V príspevku sú uvedené tiež príklady vybraných scenárov pre Hurbanovo.
This paper describes the technical information and performance of a new multi-objective chamber system enabling the control of environmental variables (e.g., temperature, CO2, air humidity, wind speed, and UV-B radiation) for understanding plant responses to climate change. Over a whole growing season, four different climate scenarios were evenly programmed into the system’s 16 chambers as ambient environment (AMB), elevated temperature (ET), elevated CO2 concentration (EC) and elevated temperature and CO2 concentration (ETC). Simultaneously, the chamber effects were assessed regarding the physiological responses and growth of a boreal perennial grass (reed canary grass, Phalaris arundinacea L.). During the growing season, the chamber system provided a wide variety of climatic conditions for air temperature (T a), relative humidity (RH) and CO2 concentration (C a) in the AMB chambers following outside conditions. The target temperature (+3.5°C) was achieved to a good degree in the ET and ETC chambers, being on average 3.3°C and 3.7°C higher than ambient conditions, respectively. The target concentration of CO2 (700 ppm) was also well achieved in the EC and ETC chambers, being on average 704 ppm and 703 ppm, respectively. The stable airflow condition inside all of the chambers provided a homogeneous distribution of gases and temperature. The decreases in RH and increases in vapour pressure deficit (VPD) in the elevated temperature chambers were also maintained at a low level. Chamber effects were observed, with some physiological and growth parameters of plants being significantly lower in the AMB chambers, compared to outside conditions. The plant growth was negatively affected by the reduced radiation inside the chambers., X. Zhou ... [et al.]., and Obsahuje bibliografii
Climate change scenarios of high quantiles of 5-day precipitation amounts (proxies for flood-generating events) over the Czech Republic are evaluated in an ensemble of high-resolution Regional Climate Model (RCM) simulations from the ENSEMBLES project. The region-of-influence method of the regional frequency analysis is applied as a pooling scheme. This means that for any single gridbox, a homogeneous region (set of gridboxes) is identified and data from that region are used when fitting the Generalized Extreme Value distribution. The climate change scenarios for the late 21st century (2070-2099) show widespread increases in high quantiles of 5-day precipitation amounts in winter, consistent with projected changes in mean winter precipitation. In summer, increases in precipitation extremes occur despite an overall drying (prevailing declines in mean summer precipitation), which may have important hydrological implications. The results for summer suggest a possible substantial change in characteristics of warm-season precipitation over Central Europe, with more severe dry as well as wet extremes. The spatial pattern of projected changes in summer precipitation extremes, with larger increases in the western part of the area and smaller changes towards east, may also point to a declining role of Mediterranean cyclones in producing precipitation extremes in Central Europe in a future climate. However, uncertainties of the climate change scenarios remain large, which is partly due to biases in reproducing precipitation characteristics in climate models, partly due to large differences among the RCMs, and partly due to factors that are poorly or not at all represented in the examined ensemble. The latter are related also to uncertainties in future emission scenarios and socio-economic development in general. and Práca analyzuje scenáre klimatickej zmeny pre vysoké kvantily 5-denných úhrnov zrážok (ktoré predstavujú možné riziko z pohľadu tvorby povodňových udalostí) na území Českej republiky, a to na základe širšej množiny simulácií z regionálnych klimatických modelov (RCM) s vysokým priestorovým rozlíšením, dostupných z projektu ENSEMBLES. Kvantily zrážkových extrémov sa odhadujú na základe metódy vplyvného regiónu, ktorá je jedným z variantov regionálnej frekvenčnej analýzy. To znamená, že pre každý gridový bod sa identifikuje jedinečný homogénny región (t.j. množina ďalších gridových bodov) a zrážkové údaje dostupné zo všetkých gridových bodov v rámci daného regiónu sa zužitkujú v procese odhadovania kvantilov využitím zovšeobecneného extremálneho rozdelenia. Scenáre klimatickej zmeny pre obdobie posledných troch dekád 21. storočia (2070-2099) naznačujú rozsiahly nárast vysokých kvantilov 5-denných úhrnov zrážok počas zimy, čo je v súlade s predpokladanými zmenami v priemerných úhrnoch zrážok za zimu. V lete sa tiež očakáva zvýšenie extrémnych úhrnov zrážok, čo môže v súvislosti s predpokladaným všeobecným úbytkom zrážok v tomto období (t.j. napriek prevažujúcemu poklesu priemerných úhrnov zrážok v lete) viesť k vážnym hydrologickým následkom. Výsledky pre leto naznačujú zásadnú zmenu v režime úhrnov zrážok v strednej Európe v teplom období roka, spojenú s častejším výskytom nepriaznivých suchých aj vlhkých extrémov. Priestorové rozdelenie predpokladaných zmien v extrémnych úhrnoch zrážok za leto - s vyšším nárastom v západných častiach skúmanej oblasti a postupne menej výrazným nárastom smerom na východ - zrejme poukazuje na slabnúcu úlohu stredomorských cyklón pri tvorbe zrážkových extrémov v strednej Európe v nastávajúcich klimatických podmienkach. Treba však podotknúť, že neurčitosť scenárov klimatickej zmeny je stále veľká, a to jednak v dôsledku nepresností v reprodukcii charakteristík úhrnov zrážok v klimatických modeloch, ďalej kvôli významným rozdielom medzi jednotlivými RCM, a nakoniec aj v dôsledku klimatických faktorov, ktoré sú slabo reprezentované, prípadne nie sú vôbec zahrnuté v analyzovanej množine výstupov klimatických modelov. Spomínané klimatické faktory takisto závisia od emisných scenárov skleníkových plynov, resp. od socio-ekonomického vývoja ľudstva vo všeobecnosti.
Projected changes of warm season (May-September) rainfall events in an ensemble of 30 regional climate model (RCM) simulations are assessed for the Czech Republic. Individual rainfall events are identified using the concept of minimum inter-event time and only heavy events are considered. The changes of rainfall event characteristics are evaluated between the control (1981-2000) and two scenario (2020-2049 and 2070-2099) periods. Despite a consistent decrease in the number of heavy rainfall events, there is a large uncertainty in projected changes in seasonal precipitation total due to heavy events. Most considered characteristics (rainfall event depth, mean rainfall rate, maximum 60-min rainfall intensity and indicators of rainfall event erosivity) are projected to increase and larger increases appear for more extreme values. Only rainfall event duration slightly decreases in the more distant scenario period according to the RCM simulations. As a consequence, the number of less extreme heavy rainfall events as well as the number of long events decreases in majority of the RCM simulations. Changes in most event characteristics (and especially in characteristics related to the rainfall intensity) depend on changes in radiative forcing and temperature for the future periods. Only changes in the number of events and seasonal total due to heavy events depend significantly on altitude.
Productivity of most improved major food crops showed stagnation in the past decades. As human population is projected to reach 9-10 billion by the end of the 21st century, agricultural productivity must be increased to ensure their demands. Photosynthetic capacity is the basic process underlying primary biological productivity in green plants and enhancing it might lead to increasing potential of the crop yields. Several approaches may improve the photosynthetic capacity, including integrated systems management, in order to close wide gaps between actual farmer’s and the optimum obtainable yield. Conventional and molecular genetic improvement to increase leaf net photosynthesis (P N) are viable approaches, which have been recently shown in few crops. Bioengineering the more efficient CC4 into C3 system is another ambitious approach that is currently being applied to the C3 rice crop. Two under-researched, yet old important crops native to the tropic Americas (i.e., the CC4 amaranths and the C3-CC4 intermediate cassava), have shown high potential P N, high productivity, high water use efficiency, and tolerance to heat and drought stresses. These physiological traits make them suitable for future agricultural systems, particularly in a globally warming climate. Work on crop canopy photosynthesis included that on flowering genes, which control formation and decline of the canopy photosynthetic activity, have contributed to the climate change research effort. The plant breeders need to select for higher P N to enhance the yield and crop tolerance to environmental stresses. The plant science instructors, and researchers, for various reasons, need to focus more on tropical species and to use the research, highlighted here, as an example of how to increase their yields., M. A. El-Sharkawy., and Obsahuje seznam literatury
In the frame of the foreseen climate global changes we analysed the physiological responses of Arbutus unedo L. to the variations of carbon dioxide concentration, leaf temperature, and irradiance by measurements of leaf gas exchange and leaf water potential performed both in field and in the laboratory. Stomatal conductance was not affected by increase of leaf temperature. The growth conditions of potted plants likely made stomata more sensitive to the variation of external parameters than naturally growing plants. The interaction between high CO2 concentration and temperature involved important down-regulation mechanisms in the metabolic pathway of the carbon fixation. From an ecological point of view, the ability of A. unedo to adapt to the field stress makes it highly competitive in the Mediterranean plant community. and M. Vitale, F. Manes.
Povrch každé planety, která má atmosféru, je zahříván nejen přímo Sluncem, ale také infračerveným zářením, které je emitováno amosférou a šíří se dolů směrem k povrchu. Na Zemi udržuje tento úkaz, známý jako skleníkový efekt, střední povrchovou teplotu zhruba o 33 K nad hodnotou, kterou by měla bez jeho působení, a tudíž je podstatný pro život na planetě.
Zářivé procesy, které jsou za skleníkový efekt odpovědné, zahrnují především minoritní složky atmosféry, jejichž podíl se může měnit buď přirozenou cestou nebo jako vedlejší důsledek činnosti lidí. Narůstání posledně jmenovaného "příspěvku" určitě podporuje obecný trend globálního ohřívání povrchu Země, i když díky problémům s modelováním složitých zpětnovazebných procesů, např. těch, které zahrnují působení vodních par, ozónu, oblačnosti a oceánů, neni jednoduché přesně předpovídat rychlost očekávaných klimatických změn a jejich lokální průběh.
Tento článek aktualizuje starší referát, v němž autor diskutoval fyzikální procesy uplatňující se při skleníkovém efektu a teoretické i experimentální práce usilující o pochopení vlivu známých i pouze očekávaných změn ve složení atmosféry na klima. V posledních deseti letech došlo k pokroku jak v oblasti získávání dat, tak i v numerických metodách modelování klimatu. Zdá se, že nové výsledky mají tendenci potvrzovat starší předpovědi pokud jde o pravěpodobnost výrazného nárůstu střední povrchové teploty planety v příštích 50-100 letech, téma však nepřestává být kontroverzní., F. W. Taylor ; přeložil Pavel Svoboda., and Obsahuje seznam literatury