The performance of the Climate version of the Regional Eta-coordinate Model （CREM）, a regional climate model developed by State Key Laboratory of Numerical modeling for Atmospheric Science and Geophysical Fluid Dyna...The performance of the Climate version of the Regional Eta-coordinate Model （CREM）, a regional climate model developed by State Key Laboratory of Numerical modeling for Atmospheric Science and Geophysical Fluid Dynamics/Institute of Atmospheric Physics （LASG/IAP）, in simulating rainfall anomalies during the ENSO decaying summers from 1982 to 2002 was evalu- ated. The added value of rainfall simulation relative to reanalysis data and the sources of model bias were studied. Results showed that the model simulated rainfall anomalies moderately well. The model did well at capturing the above-normal rainfall along the Yangtze River valley （YRV） during E1 Nifio decaying summers and the below and above-normal rainfall centers along the YRV and the Huaihe River valley （HRV）, respectively, during La Nifia decaying summers. These features were not evident in rainfall products derived from the reanalysis, indicating that rainfall simulation did add value. The main limitations of the model were that the simulated rainfall anomalies along the YRV were far stronger and weaker in magnitude than the observations during E1 Nifio decaying summers and La Nifia decaying summers, respectively. The stronger magnitude above-normal rainfall during E1 Nifio decaying summers was due to a stronger northward transport of water vapor in the lower troposphere, mostly from moisture advection. An artificial, above-normal rainfall center was seen in the region north to 35°N, which was associated with stronger northward water vapor transport. Both lower tropospheric circulation bias and a wetter model atmosphere contributed to the bias caused by water vapor transport. There was a stronger southward water vapor transport from the southern boundary of the model during La Nifia decaying summers; less remaining water vapor caused anomalously weaker rainfall in the model as compared to observations.展开更多
Watching the winds in northwest Iowa during more than 30 summers has led me to two conclusions about the local atmosphere at ground level: there is a net northward transport of heat and water taking place throughout t...Watching the winds in northwest Iowa during more than 30 summers has led me to two conclusions about the local atmosphere at ground level: there is a net northward transport of heat and water taking place throughout the summer;warm humid winds from the south continually alternate with cool dry winds from the north. The proposed northward heat transfer is consistent with the constraint, placed on the motions of the oceans and the atmosphere, of the earth’s heat balance due to the increased absorption of solar radiation at low latitudes compared to that at high latitudes. At mid-latitudes in the interior of continents, like North America, it is the job of the atmosphere alone to constantly help satisfy the global heat balance. Although qualitative in nature, the predicted northward heat flux is strongly based on frequent observations over lengthy time intervals.展开更多
目的:建立上颌窦内提升的山羊动物实验模型,比较IBS内提骨凿与Summers骨凿进行山羊上颌窦内提升的效果。方法:大量预实验对山羊上颌窦解剖分析,结合山羊CBCT对上颌窦提升位点探讨,建立上颌窦内提升的山羊动物实验模型。对18只本地山羊3...目的:建立上颌窦内提升的山羊动物实验模型,比较IBS内提骨凿与Summers骨凿进行山羊上颌窦内提升的效果。方法:大量预实验对山羊上颌窦解剖分析,结合山羊CBCT对上颌窦提升位点探讨,建立上颌窦内提升的山羊动物实验模型。对18只本地山羊36个上颌窦左右随机分为实验组与对照组,实验组运用IBS内提骨凿,对照组运用Summers骨凿,18只山羊依据上颌窦提升高度为5,8,10mm随机分为3组,每组6只羊头,统计每组实验组与对照组的穿孔数并记录穿孔时上颌窦提升的高度。结果:建立了以山羊上颌第一磨牙腭侧6-8mm的位点进行上颌窦内提升的动物实验模型。每组实验组6个上颌窦穿孔数分别为0、1、3;对照组6个上颌窦穿孔数分别为1、5、6。实验组与对照组行上颌窦内提升高度为5mm时两者安全性无明显差异[(5.00±0.00) mm vs(4.92±0.20) mm,P>0.05],实验组与对照组行上颌窦内提升高度为8mm时两者差异显著[(7.83±0.41) mm vs (6.58±1.32) mm,P<0.05],实验组与对照组行上颌窦内提升高度为10mm时两者安全性差异显著[(9.17±1.57) mm vs (6.08±0.97) mm,P<0.05]。结论:山羊上颌第一磨牙腭侧6-8mm的位点进行上颌窦内提升效果显著,当提升高度小于5mm,两者提升效果无明显差异,提升高度大于5mm,两骨凿相较而言,IBS内提骨凿较Summers骨凿有更好的提升效果及安全性。展开更多
DB 33/1015—2021《居住建筑节能设计标准》对居住建筑外墙等性能提出更严苛的要求,直接影响建筑总体造价。如何在满足现行节能标准前提下,控制初始投资成本及投资回收期具有较强现实意义。通过调研杭州市21个居住建筑项目(共227幢单体...DB 33/1015—2021《居住建筑节能设计标准》对居住建筑外墙等性能提出更严苛的要求,直接影响建筑总体造价。如何在满足现行节能标准前提下,控制初始投资成本及投资回收期具有较强现实意义。通过调研杭州市21个居住建筑项目(共227幢单体建筑),并基于Rhino和Grasshopper平台建立一典型高层住宅外墙的遗传算法优化模型。优化结果显示,外墙在采用合理形式的复合保温构造后可在降低建筑运行能耗(降幅14.46%~16.27%),将投资回收期控制在合理范围内(13.54~15.00年),可为相似建筑设计提供参考。展开更多
基金supported by the China-UK-Swiss Adapting to Climate Change in China(ACCC)Project-Climate Sciencethe Chinese Academy of Science Project under Grant KZCX2-YW-Q11-04
文摘The performance of the Climate version of the Regional Eta-coordinate Model （CREM）, a regional climate model developed by State Key Laboratory of Numerical modeling for Atmospheric Science and Geophysical Fluid Dynamics/Institute of Atmospheric Physics （LASG/IAP）, in simulating rainfall anomalies during the ENSO decaying summers from 1982 to 2002 was evalu- ated. The added value of rainfall simulation relative to reanalysis data and the sources of model bias were studied. Results showed that the model simulated rainfall anomalies moderately well. The model did well at capturing the above-normal rainfall along the Yangtze River valley （YRV） during E1 Nifio decaying summers and the below and above-normal rainfall centers along the YRV and the Huaihe River valley （HRV）, respectively, during La Nifia decaying summers. These features were not evident in rainfall products derived from the reanalysis, indicating that rainfall simulation did add value. The main limitations of the model were that the simulated rainfall anomalies along the YRV were far stronger and weaker in magnitude than the observations during E1 Nifio decaying summers and La Nifia decaying summers, respectively. The stronger magnitude above-normal rainfall during E1 Nifio decaying summers was due to a stronger northward transport of water vapor in the lower troposphere, mostly from moisture advection. An artificial, above-normal rainfall center was seen in the region north to 35°N, which was associated with stronger northward water vapor transport. Both lower tropospheric circulation bias and a wetter model atmosphere contributed to the bias caused by water vapor transport. There was a stronger southward water vapor transport from the southern boundary of the model during La Nifia decaying summers; less remaining water vapor caused anomalously weaker rainfall in the model as compared to observations.
文摘Watching the winds in northwest Iowa during more than 30 summers has led me to two conclusions about the local atmosphere at ground level: there is a net northward transport of heat and water taking place throughout the summer;warm humid winds from the south continually alternate with cool dry winds from the north. The proposed northward heat transfer is consistent with the constraint, placed on the motions of the oceans and the atmosphere, of the earth’s heat balance due to the increased absorption of solar radiation at low latitudes compared to that at high latitudes. At mid-latitudes in the interior of continents, like North America, it is the job of the atmosphere alone to constantly help satisfy the global heat balance. Although qualitative in nature, the predicted northward heat flux is strongly based on frequent observations over lengthy time intervals.
文摘目的:建立上颌窦内提升的山羊动物实验模型,比较IBS内提骨凿与Summers骨凿进行山羊上颌窦内提升的效果。方法:大量预实验对山羊上颌窦解剖分析,结合山羊CBCT对上颌窦提升位点探讨,建立上颌窦内提升的山羊动物实验模型。对18只本地山羊36个上颌窦左右随机分为实验组与对照组,实验组运用IBS内提骨凿,对照组运用Summers骨凿,18只山羊依据上颌窦提升高度为5,8,10mm随机分为3组,每组6只羊头,统计每组实验组与对照组的穿孔数并记录穿孔时上颌窦提升的高度。结果:建立了以山羊上颌第一磨牙腭侧6-8mm的位点进行上颌窦内提升的动物实验模型。每组实验组6个上颌窦穿孔数分别为0、1、3;对照组6个上颌窦穿孔数分别为1、5、6。实验组与对照组行上颌窦内提升高度为5mm时两者安全性无明显差异[(5.00±0.00) mm vs(4.92±0.20) mm,P>0.05],实验组与对照组行上颌窦内提升高度为8mm时两者差异显著[(7.83±0.41) mm vs (6.58±1.32) mm,P<0.05],实验组与对照组行上颌窦内提升高度为10mm时两者安全性差异显著[(9.17±1.57) mm vs (6.08±0.97) mm,P<0.05]。结论:山羊上颌第一磨牙腭侧6-8mm的位点进行上颌窦内提升效果显著,当提升高度小于5mm,两者提升效果无明显差异,提升高度大于5mm,两骨凿相较而言,IBS内提骨凿较Summers骨凿有更好的提升效果及安全性。
