Estimating heat flux transmission of vertical greenery ecosystem

Nurturing vegetation on building envelopes provides an innovative and eco-friendly alternative to urban greening especially in compact cities. Whereas the thermal and other benefits of green roofs have been studied intensively, green walls have received scanty attention. This study evaluates the thermodynamic transmission process of the vertical greenery ecosystem. We designed a field experiment to monitor solar radiation and weather conditions, and developed a thermodynamics transmission model to simulate heat flux and temperature variations. The model was calibrated, tested, and proved to be highly efficient. The results show that seasonal global and direct solar radiation drops to minimum in winter in January and February, and reaches maximum in summer in July and August (1168 W m⁻² for global solar radiation and 889 W m⁻² for direct solar radiation). Diffuse solar radiation attains maximum in summer (586 W m⁻²) with moderate rainfall in July and August, and minimum in winter with no rainfall in January and February. Radiation transmission of the green wall strongly correlates with canopy transmittance and reflectance (R² = 0.83). Thermal shielding effectiveness varies with orientation, with the south wall achieving a higher coefficient (0.31) than the north wall. The south wall has lower heat flux absorbance and heat flux loss than the north wall. The south wall can transfer much more heat flux through the vertical greenery ecosystem due to more intensive canopy evapotranspiration effect. The model matches the transmission properties of green wall radiation, and the model simulation fits empirical transmission results.     

A tolerability and pharmacokinetic study of adjuvant erlotinib and capecitabine with concurrent radiation in resected pancreatic cancer

BACKGROUND: Erlotinib is approved for the treatment of advanced pancreas cancer. We conducted a prospective trial to determine the safety profile and recommended phase 2 dose of erlotinib and capecitabine given concurrently with intensity-modulated radiation therapy (IMRT) in resected pancreatic cancer patients. The pharmacokinetic profile of this combination was also evaluated. METHODS: Patients with resected pancreatic adenocarcinoma received erlotinib and capecitabine concurrently with IMRT delivered at 1.8 Gy daily in 28 fractions (total = 50.4 Gy). The starting dose level (DL 1) was erlotinib 150mgdaily and capecitabine 800 mg/m² twice daily without interruption. The next lower dose level (DL -1) was erlotinib 100 mg daily and capecitabine 800 mg/m² twice daily (Monday to Friday). Plasma samples were obtained for pharmacokinetic analysis. RESULTS: Thirteen patients were enrolled in total. At DL 1, six of the seven treated patients were evaluable for toxicities. Four completed planned treatment, but all required treatment interruption or dose reduction. The dose-limiting toxicities were neutropenia, diarrhea, and rash. Six patients were subsequently enrolled to and completed planned treatment in DL-1. Themost common toxicities were fatigue, elevated liver enzymes, and anorexia. The pharmacokinetic parameters of erlotinib and OSI-420 were not significantly different in the presence or absence of capecitabine and were consistent with historical controls. CONCLUSIONS: When administered concurrently with IMRT, erlotinib 100 mg daily and capecitabine 800 mg/m² twice daily (Monday to Friday) can be administered safely in resected pancreas cancer patients, and is the recommended regimen for efficacy studies using this regimen.     

Solar radiation transmission in and around canopy gaps in an uneven-aged <Emphasis Type="Italic">Nothofagus betuloides</Emphasis> forest

The transmission of direct, diffuse and global solar radiation in and around canopy gaps occurring in an uneven-aged, evergreen Nothofagus betuloides forest during the growing season (October 2006–March 2007) was estimated by means of hemispherical photographs. The transmission of solar radiation into the forest was affected not only by a high level of horizontal and vertical heterogeneity of the forest canopy, but also by low angles of the sun’s path. The below-canopy direct solar radiation appeared to be variable in space and time. On average, the highest amount of transmitted direct solar radiation was estimated below the undisturbed canopy at the southeast of the gap centre. The transmitted diffuse and global solar radiation above the forest floor exhibited lower variability and, on average, both were higher at the centre of the canopy gaps. Canopy structure and stand parameters were also measured to explain the variation in the below-canopy solar radiation in the forest. The model that best fit the transmitted below-canopy direct solar radiation was a growth model, using plant area index with an ellipsoidal angle distribution as the independent variable (R ² = 0.263). Both diffuse and global solar radiation were very sensitive to canopy openness, and for both cases a quadratic model provided the best fit for these data (R ² = 0.963 and 0.833, respectively). As much as 75% and 73% of the variation in the diffuse and global solar radiation, respectively, were explained by a combination of stand parameters, namely basal area, crown projection, crown volume, stem volume, and average equivalent crown radius.     

Estimating mean monthly incident solar radiation on horizontal and inclined slopes from mean monthly temperatures extremes

Although satellite-borne sensors are now available to estimate cloud cover and incoming short-wave radiation across the Earth’s surface, the study of climatic variation and its impact on terrestrial and marine ecosystems involves historical analyses of data from networks of weather stations that only record extremes in temperatures and precipitation on a daily basis. Similarly, when projections are made with global atmospheric circulation models, the spatial resolution of predicted radiation is too coarse to incorporate the effects of heterogeneous topography. In this paper, we review the development and set forth a set of general equations that allow both diffuse and direct solar radiation to be estimated for each month on the basis of mean daily maximum and minimum temperatures, latitude, elevation, slope, and aspect. Adjustments for differences in slope, aspect, and elevation are made by varying the fraction of diffuse and direct solar beam radiation. To test the equations on various slopes and under different climatic conditions, we drew on high-quality radiation data recorded at a number of sites on three continents. On horizontal surfaces the set of equations predicted both direct and diffuse components of solar radiation within 1%–7% of recorded values. On slopes, estimates of monthly mean solar radiation were with 13% of observed values with a mean error of less than 2 MJ m^–2day^–1 over any given month. Received: 22 October 1999 / Revised: 14 May 2000 / Accepted: 5 June 2000     

基于机器学习算法的草地地上生物量估测——以祁连山草地为例

草地地上生物量（Aboveground Biomass,AGB）是指导畜牧业生产管理的重要指标,是草畜平衡综合分析的基础。目前,有关祁连山草地AGB反演的研究较少,且多源数据间的尺度差异问题并未得到很好的解决。为了解祁连山草地AGB的空间分布状况,利用Sentinel-2多光谱数据、无人机（Unmanned Aerial Vehicle,UAV）数据以及2021年植被生长期实测草地AGB数据实现了空天地一体化监测,通过决策树回归（Decision Tree Regression,DTR）、随机森林回归（Random Forest Regression,RFR）、梯度提升决策回归树（Gradient Boosting Regression Tree,GBRT）以及极致梯度提升（eXtreme Gradient Boosting,XGBoost）共4种算法反演草地AGB的适用性分析,利用最优模型反演了祁连山草地的AGB空间分布状况。结果表明：研究区内多种植被指数所表现出的特性有所差异。祁连山地区AGB在空间分布上呈现出由西北向东南递增的趋势,平均AGB为925.43kg/hm²。6种植被指数与实测AGB之间均表现为显著正相关,适合作为祁连山草地AGB遥感反演的指标;XGBoost模型较其它模型具有最高的R²值（0.78）和精度（74.75%）、最低的均方根误差（RMSE,99.74 kg/hm²）和平均绝对误差（MAE,71.60 kg/hm²）,模型反演效果最好;UAV数据能够提供更加详细的空间细节特征,减小Sentinel-2数据和实地采样数据间的尺度差异;因此,基于6种植被指数与祁连山草地AGB间的相关性,构建XGBoost模型反演研究区草地AGB空间分布状况是具有实践意义的。研究结果将为指导祁连山草地畜牧业的发展和维护草地生态系统的平衡提供一定的参考价值与数据支撑。     

Tradeoffs between Maize Silage Yield and Nitrate Leaching in a Mediterranean Nitrate-Vulnerable Zone under Current and Projected Climate Scenarios

Future climatic changes may have profound impacts on cropping systems and affect the agronomic and environmental sustainability of current N management practices. The objectives of this work were to i) evaluate the ability of the SALUS crop model to reproduce experimental crop yield and soil nitrate dynamics results under different N fertilizer treatments in a farmer’s field, ii) use the SALUS model to estimate the impacts of different N fertilizer treatments on NO₃^- leaching under future climate scenarios generated by twenty nine different global circulation models, and iii) identify the management system that best minimizes NO₃^- leaching and maximizes yield under projected future climate conditions. A field experiment (maize-triticale rotation) was conducted in a nitrate vulnerable zone on the west coast of Sardinia, Italy to evaluate N management strategies that include urea fertilization (NMIN), conventional fertilization with dairy slurry and urea (CONV), and no fertilization (N0). An ensemble of 29 global circulation models (GCM) was used to simulate different climate scenarios for two Representative Circulation Pathways (RCP6.0 and RCP8.5) and evaluate potential nitrate leaching and biomass production in this region over the next 50 years. Data collected from two growing seasons showed that the SALUS model adequately simulated both nitrate leaching and crop yield, with a relative error that ranged between 0.4% and 13%. Nitrate losses under RCP8.5 were lower than under RCP6.0 only for NMIN. Accordingly, levels of plant N uptake, N use efficiency and biomass production were higher under RCP8.5 than RCP6.0. Simulations under both RCP scenarios indicated that the NMIN treatment demonstrated both the highest biomass production and NO₃^- losses. The newly proposed best management practice (BMP), developed from crop N uptake data, was identified as the optimal N fertilizer management practice since it minimized NO₃^- leaching and maximized biomass production over the long term.     

An improved estimation of daily clear-sky biologically EER from broadband global solar radiation

To establish a relation between biologically effective erythemal radiation (EER) and global solar radiation, the hourly and daily clear-sky broadband (310–2,800 nm) global solar radiation (G) and spectral ultraviolet radiation incident on a horizontal surface at Esfahan, Iran (32°37′N, 51°40′E) were measured during the period 2001–2005. Good correlations at statistically significant levels between the daily values of EER and the daily G were found. The seasonal variability of EER/G is also discussed and the correction factors are determined for inclusion of vertical column ozone and solar zenith angle (SZA) cycles. The comparison of the estimated daily EER against the independent observed EER revealed that under clear sky conditions the estimations are accurate to 10% or better over SZA of 10–60° and column ozone of 250–350 Dobson. The comparison of the results with the similar works that have used shorter period of experimental data showed more accurate estimates. The deduced relations could be used to a rough estimate of the daily EER from G in arid climate regions, where there is no measured UV radiation or there are instrumental and other difficulties encountered in measuring UV radiation.     

近48a华北区太阳辐射量时空格局的变化特征

以分析华北区太阳辐射量时空格局变化特征为研究目标,应用国家气象局整编的华北地区120个气象站点48a(1961-2008)的气象资料和中国数字高程模型,对48a来华北地区太阳辐射量进行计算及验证,并对空间格局及变异特征进行了探讨,结果表明:(1)华北地区太阳辐射量的年际间变化较大,总体呈下降趋势,线性倾向值为-7.72 MJ · m^-2 · a^-1;(2)太阳辐射量由多到少突变发生在1981年,1981-2008年太阳辐射量平均值较1961-1981年降低了203.92 MJ · m^-2 · a^-1。从1981年突变年开始,华北地区太阳辐射量表现出明显的下降趋势,且在分析期内,下降的态势得到持续发生;(3)1981/1982年度发生的太阳辐射量由多到少突变,大部分地区突变幅度在150 MJ/m²以上。突变严重的华北中部和南部地区,突变值可达300 MJ/m²;(4)突变年后,华北大部分地区均表现出持续下降的态势,下降速度在6 MJ · m^-2 · a^-1以上,其中华北东北部下降严重,下降速度可达15 MJ · m^-2 · a^-1。     

Global solar radiation as the factor controlling induction of diapause in the pod midge (Dasyneura brassicae Winn.)

In this paper we examine the hypothesis that diapause induction in the polyvoltine pod midge Dasyneura brassicae Winn. (Diptera: Cecidomyiidae) is controlled by cumulative global solar radiation during the larval stage. The correlation between field observations of relative diapause for 3 years and four environmental factors (daylength, temperature, cumulative daylight time, and cumulative global solar radiation) was investigated. The cumulative global solar radiation during the larval stage clearly showed the strongest correlation with the observed relative diapause. It was estimated that larvae which cumulated less than 71.1 kWh m⁻² entered diapause. Compared to former theories on diapause induction in insects, this hypothesis explains how temperature and light can function together and, furthermore, it removes the requirement for biological clock involvement in diapause induction in insects. Received: 21 December 1996 / Accepted: 26 February 1997     

青藏高原植被生态系统垂直分布变化的情景模拟

如何模拟和揭示青藏高原植被生态系统垂直分布在全球气候变化驱动下的时空变化情景,对定量解析青藏高原陆地生态系统对气候变化响应效应具有重要意义。该论文基于Holdridge life zone （HLZ）模型,结合数字高程模型（DEM）数据,改变模型输入参数模式,发展了改进型HLZ生态系统模型。结合1981-2010（T0）时段的气候观测数据和IPCC CMIP5 RCP2.6、RCP4.5、RCP8.5三种情景2011-2040（T1）、2041-2070（T2）、2071-2100（T3）三个时段气候情景数据,实现了青藏高原植被生态系统垂直分布的时空变化情景模拟。引入生态系统平均中心时空偏移趋势模型和生态多样性指数模型,定量揭示了青藏高原植被生态系统在不同垂直带上的时空变化情景。结果显示：青藏高原共有16种植被生态系统类型;冰雪/冰原、高山潮湿苔原和亚高山湿润森林为青藏高原主要的植被生态系统类型,其面积之和占到了青藏高原总面积的56.26%;高山干苔原、亚高山潮湿森林、山地灌丛、山地湿润森林和荒漠等对气候变化的敏感性总体上高于其它类型;在T0-T3期间,青藏高原的高山湿润苔原、高山干苔原、荒漠呈持续减少趋势,平均每10年将分别减少1.96×10⁴km²、0.15×10⁴km²和1.58×10⁴km²;亚高山潮湿森林、山地湿润森林和山地灌丛呈持续增加趋势,平均每10年将分别增加3.42×10⁴km²、2.98×10⁴km²和1.19×10⁴km²;RCP8.5情景下青藏高原的植被生态系统平均中心的偏移幅度最大,RCP4.5情景下的偏移幅度次之,而RCP2.6情景下的偏移幅度最小。另外,在三种气候变化情景驱动下,青藏高原植被生态系统的生态多样性呈减少趋势。总之,未来不同情景的气候变化将直接影响青藏高原植被生态系统的时空分布格局及其生态多样性,气候变化强度越高,影响就越大,而且气候变化对青藏高原植被生态系统的影响呈现出从低海拔到高海拔递增的影响效应。     

SOLWEIG 1.0 – Modelling spatial variations of 3D radiant fluxes and mean radiant temperature in complex urban settings

The mean radiant temperature, T_mrt, which sums up all shortwave and longwave radiation fluxes (both direct and reflected) to which the human body is exposed is one of the key meteorological parameters governing human energy balance and the thermal comfort of man. In this paper, a new radiation model (SOLWEIG 1.0), which simulates spatial variations of 3D radiation fluxes and T_mrt in complex urban settings, is presented. The T_mrt is derived by modelling shortwave and longwave radiation fluxes in six directions (upward, downward and from the four cardinal points) and angular factors. The model requires a limited number of inputs, such as direct, diffuse and global shortwave radiation, air temperature, relative humidity, urban geometry and geographical information (latitude, longitude and elevation). The model was evaluated using 7 days of integral radiation measurements at two sites with different building geometries – a large square and a small courtyard in Göteborg, Sweden (57°N) – across different seasons and in various weather conditions. The evaluation reveals good agreement between modelled and measured values of T_mrt, with an overall good correspondence of R ²?=?0.94, (p?相似文献   

西安太阳总辐射时空变化特征及对城市发展的响应

根据西安辐射站太阳总辐射资料和周围23个气象台站日照百分率资料,建立1961-2009年西安市太阳总辐射资料时间序列,运用模糊聚类分析法将全市分为3个区,采取滑动t检验法进行突变检验及阶段分析,研究西安太阳总辐射的时空分布及变化特征.同时引用西安历年城区人口数据,对城区太阳总辐射与城市发展进行了相关性分析.结果表明:西安太阳总辐射具有东部多、西部次之、中部少的分布特征;1961-2009年呈波段减少的变化趋势,线性倾向率为-2.01％/10a,其中1977-1991年为显著减少阶段,以中部减少幅度最大;其间出现两次突变,突变年分别为1977年及1992年;城市发展带来大气污染物的增加,造成西安城区太阳总辐射对城市发展有较大的响应,西安城市发展对太阳总辐射季节影响上表现为冬、夏季远大于春、秋季.     

Vegetation‐mediated impacts of trends in global radiation on land hydrology: a global sensitivity study

Incident solar radiation has changed in the last 50 years, as an initial dimming trend from 1960 to approximately 1990 was followed by an ongoing brightening period, with concomitant changes in the partitioning between direct and diffuse fractions. Such radiation changes are expected to affect the global water cycle. In this study, we use the Community Land Model (CLM) to perform global offline simulations for the period 1948–2004 and study the effects of solar forcing changes on trends in evapotranspiration and runoff. The modeled components of the hydrologic cycle respond strongly to the imposed radiation changes in several regions, especially in the tropics. Exceptions are regions with soil moisture‐limited evapotranspiration regime, such as the U.S. Great Plains. In Europe and the Eastern US, the imposed 7 W m^?2 solar dimming for 1960–1990 leads to an evapotranspiration reduction of 1.5 W m^?2 or approximately 5% of the mean and an enhancement of runoff by equal percentage. In these regions, the imposed 6 W m^?2 solar brightening leads to a 3 W m^?2 increase of evapotranspiration in 1990–2004, and a runoff reduction of between 7 and 10% of the mean. Additional simulations investigating the impact of higher diffuse radiation fraction during 1960–1990 suggest mostly an increase of evapotranspiration in the tropics of 2.5 W m^?2 (3% of mean) due to increased photosynthesis from shaded leaves, but with smaller opposite effects elsewhere because of lower ground evaporation. The runoff trend resulting from the imposed radiation/aerosols effect is of the same sign and approximate relative magnitude (but larger absolute magnitude) as those calculated, in various studies, for other potential drivers of runoff change such as climate, CO₂, or land use. These results thus strengthen the claim that radiation effects on runoff are not to be neglected. Understanding the impacts of radiation on the water cycle will affect projections of river flow and freshwater availability for human consumption.     

Effect of ammonium chloride on subcellular distribution of lysosomal enzymes in human fibroblasts

Three subcellular fractions enriched in lysosomal enzyme activities have been isolated recently from human cultured fibroblasts with Percoll gradients: the dense lysosomes (DL), light lysosomes (LL), and light membranous vesicles (LM). They were shown to have different morphological, cytochemical, biochemical, and immunological properties. We now report on the dramatic but different effects of a primary amine, NH4Cl, on these subfractions. The lysosomes, as detected with a specific ultrastructural cytochemical stain for the lysosomal enzyme, arylsulfatase A, were swollen significantly in all these fractions, increasing their volumes by 64% (DL), 53% (LL), and 95% (LM), respectively. When arylsulfatase A enzyme activity was monitored, about half of the DL content was diverted to the LL. However, when newly synthesized arylsulfatase A enzyme protein was monitored with metabolic labeling and immunoprecipitation, about 80% of the enzyme protein was depleted from both the DL and LL. In contrast, neither the enzyme activity nor the newly synthesized enzyme protein of arylsulfatase A was greatly altered in the LM fraction by the treatment. Since primary amines caused newly synthesized lysosomal enzymes to diverge from the lysosomal route to a secretory pathway, it was deduced that (i) the LM fraction corresponded to a prelysosomal compartment whose lysosomal enzyme content was not affected by the amine and was thus proximal to the point of diversion between the secretory and lysosomal pathways; (ii) the LL and DL fractions were distal to the point of diversion since both fractions were depleted of their newly synthesized lysosomal enzyme; and (iii) the sorting of newly synthesized lysosomal enzyme may be different from that of the preexisting pool of the same enzyme since the LL fraction was depleted of its newly synthesized enzyme protein while accumulating excessive enzyme activity.     

Coral Reef Habitat Response to Climate Change Scenarios

Coral reef ecosystems are threatened by both climate change and direct anthropogenic stress. Climate change will alter the physico-chemical environment that reefs currently occupy, leaving only limited regions that are conducive to reef habitation. Identifying these regions early may aid conservation efforts and inform decisions to transplant particular coral species or groups. Here a species distribution model (Maxent) is used to describe habitat suitable for coral reef growth. Two climate change scenarios (RCP4.5, RCP8.5) from the National Center for Atmospheric Research’s Community Earth System Model were used with Maxent to determine environmental suitability for corals (order Scleractinia). Environmental input variables best at representing the limits of suitable reef growth regions were isolated using a principal component analysis. Climate-driven changes in suitable habitat depend strongly on the unique region of reefs used to train Maxent. Increased global habitat loss was predicted in both climate projections through the 21^st century. A maximum habitat loss of 43% by 2100 was predicted in RCP4.5 and 82% in RCP8.5. When the model is trained solely with environmental data from the Caribbean/Atlantic, 83% of global habitat was lost by 2100 for RCP4.5 and 88% was lost for RCP8.5. Similarly, global runs trained only with Pacific Ocean reefs estimated that 60% of suitable habitat would be lost by 2100 in RCP4.5 and 90% in RCP8.5. When Maxent was trained solely with Indian Ocean reefs, suitable habitat worldwide increased by 38% in RCP4.5 by 2100 and 28% in RCP8.5 by 2050. Global habitat loss by 2100 was just 10% for RCP8.5. This projection suggests that shallow tropical sites in the Indian Ocean basin experience conditions today that are most similar to future projections of worldwide conditions. Indian Ocean reefs may thus be ideal candidate regions from which to select the best strands of coral for potential re-seeding efforts.     

Initial contact and toe off event identification for rearfoot and non-rearfoot strike pattern treadmill running at different speeds

The purpose of this study was to determine the validity of kinematic based initial contact (IC) and toe-off (TO) identification algorithms for rearfoot and non-rearfoot runners across a broad range of treadmill running speeds. 14 healthy active participants completed six 20–60 s treadmill running trials at 6 speeds: 2.24, 2.68, 3.13, 3.58, 4.02, and 4.48 ms⁻¹. 3D kinematic data were collected for the last 20 s of each trial. Force plates (FP) were used as the gold standard to determine ICFP and TOFP for each step. Three algorithms for finding IC, IC_Milner, IC_Alvim, IC_Alvim-mod, and one algorithm for finding toe off, TO_Fellin, were chosen for analysis. Root mean square errors (RMSE) and difference scores with 95% confidence intervals were computed for IC, TO and stance time (ST). IC_Alvim RMSE ranged from 0.175 to 0.219 s. ST_Alvim RMSE ranged from 0.168 to 0.216 s. IC_Alvim-mod RMSE ranged from 0.105 to 0.131 s. ST_Alvim-mod RMSE ranged from 0.108 to 0.129 s. IC_Milner RMSE ranged 0.012 to 0.015 s. ST_Milner RMSE ranged 0.019 to 0.024 s. IC_Milner accuracy was inversely related to speed. IC_Milner corrected with a linear regression equation reduced differences to- 0.006 ± 0.012 s with 86% of foot strikes identified within 20 ms and 58% with 10 ms. TO_Fellin RMSE ranged from 0.012 to 0.016 s. IC_Milner adjusted for speed and TO_Fellin can be used to predict IC and TO within a broad range of treadmill running speeds (2.24–4.48 ms⁻¹) and for rearfoot and non-rearfoot strikers.     

Calculating solar and longwave radiation for a Mediterranean lake under various weather conditions

Two years of hourly measurements of global solar radiation and downward longwave radiation were used to estimate the radiative balance of Lake Banyoles, a small karstic Mediterranean lake. The performance of several empirical estimation equations on an hourly and a daily basis were evaluated taking into account various meteorological conditions. The new coefficients in the formulae for the effective emittance, which have been derived from meteorological data, demonstrate that these coefficients strongly depend on the radiation climate of the respective area. In the Mediterranean climate of Lake Banyoles, changes in wind direction and relative humidity after the vertical distribution of vapour pressure beneath the cloud layer. Different median experimental errors were found depending on the time scale and cloud cover. Comparison of global solar radiation measured at Banyoles with estimated values shows good agreement for clear skies, especially for daily means. On a daily scale, the root mean squared (r.m.s.) error was found to be 8% for solar radiation and 12% for longwave radiation. On an hourly scale, different r.m.s. errors were obtained depending on the degree of cloud cover.     

Analysis of photosynthetically active radiation under various sky conditions in Wuhan,Central China

Observations of photosynthetically active radiation (PAR) and global solar radiation (G) at Wuhan, Central China during 2005–2012 were first reported to investigate PAR variability at different time scales and its PAR fraction (F _p) under different sky conditions. Both G irradiances (I _g) and PAR irradiances (I _p) showed similar seasonal features that peaked in values at noon during summer and reached their lower values in winter. F _p reached higher values during either sunrise or sunset; lower values of F _p appeared at local noon because of the absorption effects of water vapor and clouds on long-wave radiation. There was an inverse relationship between clearness index (K _t) and F _p; the maximum I _p decreased by 22.3 % (39.7 %) when sky conditions changed from overcast to cloudless in summer (winter); solar radiation was more affected by cloudiness than the seasonal variation in cloudy skies when compared with that in clear skies. The maximum daily PAR irradiation (R _p) was 11.89 MJ m^?2 day^?1 with an annual average of 4.85 MJ m^?2 day^?1. F _p was in the range of 29–61.5 % with annual daily average value being about 42 %. Meanwhile, hourly, daily, and monthly relationships between R _p and G irradiation (R _g) under different sky conditions were investigated. It was discovered that cloudy skies were the dominated sky condition in this region. Finally, a clear-sky PAR model was developed by analyzing the dependence of PAR irradiances on optical air mass under various sky conditions for the whole study period in Central China, which will lay foundations for ecological process study in the near future.     

2020—2050年CO2施肥效应促进全球陆地生态系统碳吸收

CO₂施肥效应是全球变绿的主要原因,随着大气中CO₂浓度的持续增加,预估未来气候变化条件下,CO₂施肥效应对陆地生态系统的影响对减缓全球气候变化具有重大意义。基于未来气候情景数据和Farquhar模型,并结合生态过程模型BEPS(Boreal Ecosystem Productivity Simulator),定量化研究2020—2050年CO₂施肥效应对全球叶面积指数(LAI)和总初级生产力(GPP)的影响。研究结果显示2020—2050年,在RCP2.6、RCP4.5和RCP8.5气候情景下,CO₂施肥效应导致的LAI年际变化趋势分别为0.002、0.003和0.005 m^-2m^-2a^-1;三个气候情景下CO₂施肥效应对LAI的影响为CO₂每增加0.1%,LAI平均增加约8.1%—9.2%,由此导致GPP对应增加7.9%—14.6%;由CO₂施...     

Facility for studying the effects of elevated carbon dioxide concentration and increased temperature on crops

The requirements for the experimental study of the effects of global climate change conditions on plants are outlined. A semi-controlled plant growth facility is described which allows the study of elevated CO₂ and temperature, and their interaction on the growth of plants under radiation and temperature conditions similar to the field. During an experiment on winter wheat (cv. Mercia), which ran from December 1990 through to August 1991, the facility maintained mean daytime CO₂ concentrations of 363 and 692 cm³ m^?3 for targets of 350 and 700 cm³ m^?3 respectively. Temperatures were set to follow outside ambient or outside ambient +4°C, and hourly means were within 0.5°C of the target for 92% of the time for target temperatures greater than 6°C. Total photosynthetically active radiation incident on the crop (solar radiation supplemented by artifieal light with natural photoperiod) was 2% greater than the total measured outside over the same period.