Black carbon （BC） aerosols can strongly absorb solar radiation in very broad spectral wavebands, from the visible to the infrared. As a potential factor contributing to global warming, BC aerosols not only directly ...Black carbon （BC） aerosols can strongly absorb solar radiation in very broad spectral wavebands, from the visible to the infrared. As a potential factor contributing to global warming, BC aerosols not only directly change the radiation balance of the earth-atmosphere system, but also indirectly affect global or regional climate by acting as cloud conden- sation nuclei or ice nuclei to alter cloud mierophysical properties. Here, recent progresses in the studies of radiative forcing due to BC and its climate effects are reviewed. The uncertainties in current researches are discussed and some suggestions are provided for future investigations.展开更多
In this study, a special method is proposed for detecting aerosols over land by analyzing satellitemeasured far IR radiation at three channels, 8.7, 11.5, and 12.5 lain. Sensitivity tests revealed that the behavioral ...In this study, a special method is proposed for detecting aerosols over land by analyzing satellitemeasured far IR radiation at three channels, 8.7, 11.5, and 12.5 lain. Sensitivity tests revealed that the behavioral features of radiative brightness temperatures （BTs） at these three channels with increasing optical depth are different among different types of aerosols. Analyzing how BTs and their differences, xBT （BT11.5-BT12.5） and YBT （BT8.7-BT11.5）, behave with varying optical depth can help to qualitatively distinguish among aerosols and semi-quantitatively estimate their optical thicknesses. In addition, the authors found that the vertical density profile of aerosols has little impact on this method.展开更多
Two channels of the Cloud Aerosol Polarimetric Imager,onboard the TanSat-Chinese carbon dioxide observation satellite,are designed to detect the polarization state of radiation reflected by the earth-atmosphere system...Two channels of the Cloud Aerosol Polarimetric Imager,onboard the TanSat-Chinese carbon dioxide observation satellite,are designed to detect the polarization state of radiation reflected by the earth-atmosphere system in a single-viewing angle.Aiming to understand how the earth and atmospheric parameters affect the polarization state of radiation,we conduct a sensitivity analysis of the polarized reflectance at the top of atmosphere(TOA)with respect to the aerosol microphysical parameters,atmospheric profiles,and surface polarization properties.It is found that(1)the TOA polarization reflectance at 0.66 lm is most sensitive to the real part of the aerosol complex refractive index,the mean radius of the fine mode aerosol particles,as well as atmospheric pressure and temperature profiles;(2)the TOA polarization reflectance at 1.64 lm is sensitive to the volume ratio between the coarse mode and fine mode particles as well,but it is not sensitive to atmospheric profiles;and(3)surface polarization properties have a relatively weak influence on the TOA polarization reflectance at both 0.66 and 1.64 lm.展开更多
The warming over the Tibetan Plateau(TP) is very significant during last 30 years,but the thermal forcing has been weakened.The thermal weakening is attributed mainly to the enhancement of the TOA(top of atmosphere) o...The warming over the Tibetan Plateau(TP) is very significant during last 30 years,but the thermal forcing has been weakened.The thermal weakening is attributed mainly to the enhancement of the TOA(top of atmosphere) outgoing radiation.This enhancement is opposite to the greenhouse-gas-induced weakening of the global mean TOA outgoing radiation and is also unable to be explained by the observed decrease of total cloud cover.This study presents the importance of cloud height change and the warming over the TP in modulating the TOA radiation budget and thus the thermal forcing during spring and summer.On the basis of surface observations and satellite radiation data,we found that both the TOA outgoing shortwave radiation and longwave radiation were enhanced during this period.The former enhancement is due mainly to the increase of low-level cloud cover,which has a strong reflection to shortwave radiation,especially in summer.The latter enhancement is caused mainly by the planetary warming,and it is further enhanced by the decrease of total cloud cover in spring,as clouds extinguish outgoing longwave radiation emitted from the land surface.Therefore,the radiative cooling enhancement and thus the thermal weakening over the TP is a response of the earth-atmosphere system to the unique change of cloud cover configuration and the rapid warming of the land surface.However,these trends in cloud cover and TOA outgoing radiation are not well represented in four reanalyses.展开更多
In this paper,the long time behaviors of non-autonomous evolution system describing geophysical flow within the earth are studied.The uniqueness and existence of the solution to the evolution system and the existence ...In this paper,the long time behaviors of non-autonomous evolution system describing geophysical flow within the earth are studied.The uniqueness and existence of the solution to the evolution system and the existence of uniform attractor are proven.Moreover,the upper bounds of the uniform attractor's hausdorff and Fractal dimensions are obtained.展开更多
Atlantic thermohaline circulation(THC) is a key component of the Earth Climate System and identification of its changes during the 20th Century is critical to the understanding of its variation characteristics and the...Atlantic thermohaline circulation(THC) is a key component of the Earth Climate System and identification of its changes during the 20th Century is critical to the understanding of its variation characteristics and the corresponding climatic impacts.Previous researches have been inconclusive,with the results varying depending on the approach used to measure THC.The results for the two established approaches for measurement of the phenomenon(direct observation and indirect reconstruction) are contradictive(weakening and non-weakening),and their credibility needs improving.Based on the tight relationship between THC anomaly and "see-saw" intensities of Sea Surface Temperature(SST) and Surface Air Temperature(SAT),we first diagnose their quantitative relationship in the model experiments,which is corresponding to its two possible scenarios,and then reconstruct the changes of THC during the 20th Century respectively with multiple observed datasets of SST and SAT.Model results show that THC anomaly and SST/SAT "see-saw" intensities are well correlated in timescales longer than 10/40 years under scenarios of weakening/non-weakening respectively.Two kinds of reconstructions here are consistent with each other,and we propose that THC has undergone a 2-cycle oscillation with inter-decadal scale since the Industrial Revolution with a magnitude of about 1 Sv.The transformation times of decadal trend are around the mid-1910s,the 1940s,and the mid-1970s.This research further validates the main results of previous reconstructions,and points out that THC does not have a long-term weakening during the 20th Century.展开更多
基金financially supported by the National Basic Research Program of China(2011CB403405 and 2010CB955608)the Public Meteorology Special Foundation of MOST(GYHY200906020)
文摘Black carbon （BC） aerosols can strongly absorb solar radiation in very broad spectral wavebands, from the visible to the infrared. As a potential factor contributing to global warming, BC aerosols not only directly change the radiation balance of the earth-atmosphere system, but also indirectly affect global or regional climate by acting as cloud conden- sation nuclei or ice nuclei to alter cloud mierophysical properties. Here, recent progresses in the studies of radiative forcing due to BC and its climate effects are reviewed. The uncertainties in current researches are discussed and some suggestions are provided for future investigations.
基金supported by the National Basic Research Program of China (Grant No. 2006CB403705)
文摘In this study, a special method is proposed for detecting aerosols over land by analyzing satellitemeasured far IR radiation at three channels, 8.7, 11.5, and 12.5 lain. Sensitivity tests revealed that the behavioral features of radiative brightness temperatures （BTs） at these three channels with increasing optical depth are different among different types of aerosols. Analyzing how BTs and their differences, xBT （BT11.5-BT12.5） and YBT （BT8.7-BT11.5）, behave with varying optical depth can help to qualitatively distinguish among aerosols and semi-quantitatively estimate their optical thicknesses. In addition, the authors found that the vertical density profile of aerosols has little impact on this method.
基金supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDA05040000)the National High Technology Research and Development Program of China(SQ2010AA1221583001)the National Natural Science Foundation of China(40775002,41175020 and 41375008)
文摘Two channels of the Cloud Aerosol Polarimetric Imager,onboard the TanSat-Chinese carbon dioxide observation satellite,are designed to detect the polarization state of radiation reflected by the earth-atmosphere system in a single-viewing angle.Aiming to understand how the earth and atmospheric parameters affect the polarization state of radiation,we conduct a sensitivity analysis of the polarized reflectance at the top of atmosphere(TOA)with respect to the aerosol microphysical parameters,atmospheric profiles,and surface polarization properties.It is found that(1)the TOA polarization reflectance at 0.66 lm is most sensitive to the real part of the aerosol complex refractive index,the mean radius of the fine mode aerosol particles,as well as atmospheric pressure and temperature profiles;(2)the TOA polarization reflectance at 1.64 lm is sensitive to the volume ratio between the coarse mode and fine mode particles as well,but it is not sensitive to atmospheric profiles;and(3)surface polarization properties have a relatively weak influence on the TOA polarization reflectance at both 0.66 and 1.64 lm.
基金supported by the Strategic Priority Research Program(B) of the Chinese Academy of Sciences(Grant No.XDB03030300)Global Change Program of Ministry of Science and Technology of China(Grant No.2010CB951703)the National Natural Science Foundation of China(Grant Nos.41190083,41325019)
文摘The warming over the Tibetan Plateau(TP) is very significant during last 30 years,but the thermal forcing has been weakened.The thermal weakening is attributed mainly to the enhancement of the TOA(top of atmosphere) outgoing radiation.This enhancement is opposite to the greenhouse-gas-induced weakening of the global mean TOA outgoing radiation and is also unable to be explained by the observed decrease of total cloud cover.This study presents the importance of cloud height change and the warming over the TP in modulating the TOA radiation budget and thus the thermal forcing during spring and summer.On the basis of surface observations and satellite radiation data,we found that both the TOA outgoing shortwave radiation and longwave radiation were enhanced during this period.The former enhancement is due mainly to the increase of low-level cloud cover,which has a strong reflection to shortwave radiation,especially in summer.The latter enhancement is caused mainly by the planetary warming,and it is further enhanced by the decrease of total cloud cover in spring,as clouds extinguish outgoing longwave radiation emitted from the land surface.Therefore,the radiative cooling enhancement and thus the thermal weakening over the TP is a response of the earth-atmosphere system to the unique change of cloud cover configuration and the rapid warming of the land surface.However,these trends in cloud cover and TOA outgoing radiation are not well represented in four reanalyses.
基金This research is supported by the Special Funds for Major State Basic Research Projects(G1999032801) by the Natural Science Foundation of China with Grant No.19671067 and 10001028.
文摘In this paper,the long time behaviors of non-autonomous evolution system describing geophysical flow within the earth are studied.The uniqueness and existence of the solution to the evolution system and the existence of uniform attractor are proven.Moreover,the upper bounds of the uniform attractor's hausdorff and Fractal dimensions are obtained.
基金supported by National Basic Research Program of China(Grant No. 2012CB955200)National Natural Science Foundation of China(Grant Nos.41130105,40776017)+2 种基金Open Project of KLME,NUIST(Grant No. LLME0507)Special Public Sector Research of CMA,China(Grant No. GYHY200906016)a project funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions(PAPD)
文摘Atlantic thermohaline circulation(THC) is a key component of the Earth Climate System and identification of its changes during the 20th Century is critical to the understanding of its variation characteristics and the corresponding climatic impacts.Previous researches have been inconclusive,with the results varying depending on the approach used to measure THC.The results for the two established approaches for measurement of the phenomenon(direct observation and indirect reconstruction) are contradictive(weakening and non-weakening),and their credibility needs improving.Based on the tight relationship between THC anomaly and "see-saw" intensities of Sea Surface Temperature(SST) and Surface Air Temperature(SAT),we first diagnose their quantitative relationship in the model experiments,which is corresponding to its two possible scenarios,and then reconstruct the changes of THC during the 20th Century respectively with multiple observed datasets of SST and SAT.Model results show that THC anomaly and SST/SAT "see-saw" intensities are well correlated in timescales longer than 10/40 years under scenarios of weakening/non-weakening respectively.Two kinds of reconstructions here are consistent with each other,and we propose that THC has undergone a 2-cycle oscillation with inter-decadal scale since the Industrial Revolution with a magnitude of about 1 Sv.The transformation times of decadal trend are around the mid-1910s,the 1940s,and the mid-1970s.This research further validates the main results of previous reconstructions,and points out that THC does not have a long-term weakening during the 20th Century.
