ALGEBRAIC SOLITARY ROSSBY WAVE IN THE ATMOSPHERE Õýѹ´óÆøÖеĴúÊýRossby¹ÂÁ¢²¨ ¶Ì¾äÀ´Ô´
Probe of Organic Vapor Pollutants in the Atmosphere of Changchun City ³¤´ºÊÐ´óÆøÆøÏàÓлúÎÛȾÎï̽²é ¶Ì¾äÀ´Ô´
Study on the propagation of high-power Iaser beam in the atmosphere ¸ß¹¦Âʼ¤¹âÊø½üµØÃæ´óÆø´«ÊäÑо¿ ¶Ì¾äÀ´Ô´
Concentration of Ozone in the Atmosphere ´óÆøÖеijôÑõŨ¶È ¶Ì¾äÀ´Ô´
A Electrochemical Measurement of the Vertical Distribution of Ozone in the Atmosphere ´óÆø³ôÑõ´¹Ö±·Ö²¼µÄµç»¯Ñ§²âÁ¿ ¶Ì¾äÀ´Ô´
ENVELOPE SOLITARY ROSSBY WAVESIN THE ATMOSPHERE ¡ª¡ªTHE EFFECT OF LATITUDE
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Determination of average daily COconcentration in the atmosphere byinfiltration sampling tool without pump
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PARAMETERIZATION OF SOLAR RADIATIVE FLUX CALCULATION IN THE ATMOSPHERE
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Study on the Atmosphere Pollution by SO_2 during Processing of Zirantong ×ÔÈ»ÍÅÚÖÆ¹ý³ÌÖдóÆøÎÛȾÎïSO_2µÄÑо¿ ¶Ì¾äÀ´Ô´
Fuzzy Decision and the Atmosphere Environmental Quality Assessment Ä£ºý¾ö²ßÓë´óÆø»·¾³ÖÊÁ¿ÆÀ¼Û ¶Ì¾äÀ´Ô´
Numerical Experiment on the Formation of 40-60 Day Low-FrequencyOscillation in the Atmosphere
´óÆøÖÐ40¡ª60ÌìµÍƵÕñµ´ÐγɵÄÊýÖµÊÔÑé ¶Ì¾äÀ´Ô´
Influence of Dispersion Effects of Transient Eddies on Energy Transport in the Atmosphere ƵɢЧӦ¶Ô×ÔÓÉ´óÆøÄÜÁ¿ÊäË͵ÄÓ°Ïì ¶Ì¾äÀ´Ô´
Oxidation of SO_2 on the Surface of Particles in the Atmosphere, ´óÆøÖÐSO_2µÄ¹ÌÏàÑõ»¯Ñо¿ ¶Ì¾äÀ´Ô´
Distribution Pattern of Polycyclic Aromatic Hydrocarbons in the Atmosphere in Huhhot City.
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STUDIES ON AEROSOL CHEMISTRY IN THE ATMOSPHERE OVER OCEANS ¢ò. CHARACTERISTICS OF SOURCE ELEMENTAL TRACERS »·Çòº£Ñó´óÆøÆøÈܽº»¯Ñ§Ñо¿ ¢ò.À´Ô´Ê¾×ÙÔªËØµÄÌØÕ÷ ¶Ì¾äÀ´Ô´
NONLINEAR ROSSBY WAVES IN THE ATMOSPHERE AND OCEANS º£ÑóºÍ´óÆøÖеķÇÏßÐÔRossby²¨ ¶Ì¾äÀ´Ô´
A SPECIAL FORM OF NONLINEAR KELVIN WAVE IN THE ATMOSPHERE ´óÆøÖзÇÏßÐÔKelvin²¨µÄÒ»¸öÌØÊâÐÎ̬ ¶Ì¾äÀ´Ô´
Study of Aqueous-phase Oxidation for SO_2 in the Atmosphere ´óÆøÖÐSO_2µÄÒºÏàÑõ»¯Ñо¿ ¶Ì¾äÀ´Ô´
Using Gas Chromatography to Calculate the Amount of CO_2 in the Atmosphere ÓÃÆøÏàÉ«Æ×¾«È·²â¶¨´óÆøÖеÄCO_2 ¶Ì¾äÀ´Ô´
A Study of Aerosol Chemistry in the Atmosphere over Oceans Part-¢ó: Forms and Air-Sea Fluxes of Metal
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Impact of rising CO_2 in the atmosphere on ecosystem. ´óÆøCO_2Ôö¼Ó¶ÔÉú̬ϵͳµÄÓ°Ïì ¶Ì¾äÀ´Ô´
CALCULATIONS OF RAMAN SCATTERING FOR HIGH POWER LASER BEAMS IN THE ATMOSPHERE
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STUDY ON EMISSION CHARACTERISTICS OF NONMETHANE HYDROCARBONS FROM ANTHROPOGENIC SOURCES IN THE ATMOSPHERE OF BEIJING ±±¾©µØÇø´óÆøÖзǼ×Íé̼Ç⻯ºÏÎNMHC£©µÄÈËΪԴÅÅ·ÅÌØÕ÷Ñо¿ ¶Ì¾äÀ´Ô´
ADVANCES IN GLOBAL MONITORING OF CO_2 CONCENTRATION IN THE ATMOSPHERE
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A Possible Extinction Mechanism of Solar Ultraviolet Radiation by Water Vapour in the Atmosphere
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NUMERICAL CALCULATION OF NONLINEAR PROBLEM OF HIGH ENERGY LASER PROPAGATION IN THE ATMOSPHERE ¸ßÄܼ¤¹â´óÆø´«Êä·ÇÏßÐÔÎÊÌâµÄÊýÖµ¼ÆËã
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Interactions of Solitary Waves in the Atmosphere ´óÆøÖйÂÁ¢²¨µÄÏ໥×÷Óà ¶Ì¾äÀ´Ô´
ON PROBLEMS OF HIGHLY TRUNCATED LOW-SPECTRAL MODEL IN STUDIES OF MULTIPLE EQUILIBRIA IN THE ATMOSPHERE ´óÆøÆ½ºâ̬Ñо¿ÖÐ¸ß½Ø¶ÏµÍÆ×ģʽµÄÎÊÌ⠶̾äÀ´Ô´
Acoustic remote sensing of the atmosphere ´óÆøÉùÒ£¸Ð ¶Ì¾äÀ´Ô´
Accumulation Frequency Distribution and Pollution Tendency of SO_2 Concentration of the Atmosphere in Taiyuan
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EFFECTS OF CO_2 CONTENT INCREASING IN THE ATMOSPHERE ON AGRICULTURAL PRODUCTION IN CHINA
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Study on Monitoring the Daily Average Concentration of SO 2 in the Atmosphere through Successive Sampling and Discontinuous Sampling
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Sources Analysis of Marine Aerosol in the Atmosphere at Dalian Sea Area ´óÁ¬º£Óò´óÆøÆøÈܽºÎïÖÊÀ´Ô´·ÖÎö ¶Ì¾äÀ´Ô´
Determination of Trace Total Gaseous Mercury in the Atmosphere Using Two stage Gold Amalgamation Cold Vapor Absorption Spectrometry Method.
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Diffusion Welding Between Al-Sn Alloy and Other Materials in the Atmosphere Al-SnºÏ½ðÓëÆäËü²ÄÁÏÔÚ´óÆøÖеÄÀ©É¢º¸½Ó ¶Ì¾äÀ´Ô´
The monitoring analysis of 8 week period of polybrominated diphenyl ethers (PBDEs) in the atmosphere of Pearl River Delta region was made using PUF passive sampling technique, to study the PBDEs content and distribution of the region.
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The PBDEs content of Hong Kong was 92~420pg/m3, with average value of 200pg/m3, in which the contents in High st (420pg/m3) and in Kwung tong (325pg/m3) were high relatively; the use of large amount of PBDEs burning resistive agent in history might be the main source of PBDEs residual in the atmosphere of Hong Kong region.
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Kwungtong(325pg/m3)µÄPBDEsº¬Á¿½Ï¸ß,ÀúÊ·ÉÏ´óÁ¿PBDEs×èȼ¼ÁµÄʹÓÿÉÄÜÊÇÏã¸ÛµØÇø´óÆøÖÐPBDEs²ÐÁôµÄÖ÷ÒªÀ´Ô´. ¶Ì¾äÀ´Ô´
On the basis of analyzing the strength state of the dust particle in the atmosphere,the theoretical research and numerical simulation were made by studying the arising and velocity trail of the dust which is on the surface of the dust source.
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Monitoring of black carbon particles in the atmosphere in Beijing area was conducted during the period of 1996-2001. Monitoring method and some results on concentration of black carbon aerosols and its variations are given and discussed in this paper.
1992Äê¼°1996¡«2001Äê¶Ô±±¾©µØÇø´óÆøÖеĺÚ̼Á£×Ó½øÐÐÁ˽ÏϵͳµÄ¼à²âÑо¿,±¾ÎÄÖØµã½éÉÜÁËÑо¿·½·¨,²¢Ê״θø³öÁ˱±¾©µØÇø´óÆøÖкÚÌ¼ÆøÈܽºÅ¨¶È¼°Æä±ä»¯µÄÒ»°ãÌØÕ÷,ÌÖÂÛÁ˱±¾©µØÇø´óÆøÖкÚ̼Á£×ӵı³¾°Å¨¶ÈÖµµÈ¡£ ¶Ì¾äÀ´Ô´
Results Go up along with the elevation steps degree to press with atmosphere, the atmosphere oxygen presses separately of lower, obvious increment(P<0.01) of the serum content sVCAM-1,the NO and level of NOS lower obviously.
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(P<0.01)The related analysis express that the content sVCAM-1 and the atmosphere oxygens press to present separately obvious positive related(r=0.795,P<0.01),the NO and level of NOS and the atmosphere oxygens press to present separately obvious negative related. (r=-0.689,P<0.01,r=-0.652,P<0.01) .
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This calculation method for calculating the atmosphere transmittance of 3. 0~ 12. 0¦Ìm is programmed under any atmosphere condition.
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Summary of greenhouse gases World Resource Center (WDCGG) for the 1991-2004 year Korea of Tae-ahn Peninsula, Mongolia of Ulaan Uu, and China of Waliguan station began monitoring atmospheric greenhouse gas stations, carbon dioxide (CO2) and methane (CH4) data, this study nearly 15 years in East Asia, both atmospheric concentrations of greenhouse gases, Meanwhile analysis expounded the atmosphere of greenhouse gases both trends, as well as causing such changes causes.
ÀûÓÃÎÂÊÒÆøÌåÊÀ½ç×ÊÁÏÖÐÐÄ(WDCGG)ÌṩµÄ1991-2004ÄêµÄKoreaofTae-ahnPeninsula(º«¹ú)¡¢MongoliaofUlaanUu(ÃɹÅ)ÒÔ¼°ÖйúµÄÍßÀï¹ØÕ¾¼à²âµÄ´óÆøÎÂÊÒÆøÌå¶þÑõ»¯Ì¼(CO2)ºÍ¼×Íé(CH4)µÄÊý¾Ý×ÊÁÏ,±¾ÎÄÑо¿Á˽ü15Äê¶«ÑǵØÇø´óÆøÖÐÕâÁ½ÖÖÎÂÊÒÆøÌåµÄŨ¶ÈÌØÕ÷,ͬʱ·ÖÎö²ûÊöÁË´óÆøÖÐÕâÁ½ÖÖÎÂÊÒÆøÌåµÄ±ä»¯Ç÷ÊÆ,ÒÔ¼°Ôì³ÉÕâÖֱ仯µÄ³ÉÒò¡£