Retrieval of near-surface sulfur dioxide (SO2) concentrations at a
... spectrum onto the SO2 signature, giving more importance to IASI channels less influenced by interfering parameters. Practically, y and S are built from a sufficiently large sample of SO2 -free IASI spectra to include the global atmospheric variability in the absence of SO2 (see Sects. 2.2 and 2.3). ...
... spectrum onto the SO2 signature, giving more importance to IASI channels less influenced by interfering parameters. Practically, y and S are built from a sufficiently large sample of SO2 -free IASI spectra to include the global atmospheric variability in the absence of SO2 (see Sects. 2.2 and 2.3). ...
- ISP 205, sec 1 - Visions of the
... of the four jovian planets in our solar system? 27. A They lack solid surfaces. B They are much more massive then any of the terrestrial planets. C They are higher in average density than are the terrestrial planets. D They are composed of mainly hydrogen, helium, and hydrogen compounds. Answer for ...
... of the four jovian planets in our solar system? 27. A They lack solid surfaces. B They are much more massive then any of the terrestrial planets. C They are higher in average density than are the terrestrial planets. D They are composed of mainly hydrogen, helium, and hydrogen compounds. Answer for ...
03.06 Near Ground Ozone (Edition 1993)
... different layers of the atmosphere as well as its effect on living and inanimate environment are elucidated in the schematic depiction of Map 03.06.1. Production and destruction of ozone as well as the action of this pollutant gas are greatly dependent on the respective weather conditions. There are ...
... different layers of the atmosphere as well as its effect on living and inanimate environment are elucidated in the schematic depiction of Map 03.06.1. Production and destruction of ozone as well as the action of this pollutant gas are greatly dependent on the respective weather conditions. There are ...
03.06 Near Ground Ozone (Edition 1993)
... different layers of the atmosphere as well as its effect on living and inanimate environment are elucidated in the schematic depiction of Map 03.06.1. Production and destruction of ozone as well as the action of this pollutant gas are greatly dependent on the respective weather conditions. There are ...
... different layers of the atmosphere as well as its effect on living and inanimate environment are elucidated in the schematic depiction of Map 03.06.1. Production and destruction of ozone as well as the action of this pollutant gas are greatly dependent on the respective weather conditions. There are ...
The vertical distribution of thin features over the Arctic
... pathways through which pollution transport and distribution can take place from different regions in the northern hemisphere. Arctic haze is the manifestation of such transport of pollutants from the mid-latitudes during winter and spring seasons. These pollutants are of mainly anthropogenic origin ...
... pathways through which pollution transport and distribution can take place from different regions in the northern hemisphere. Arctic haze is the manifestation of such transport of pollutants from the mid-latitudes during winter and spring seasons. These pollutants are of mainly anthropogenic origin ...
The role of ammonia in plant physiology
... 6.6 µg m3 – 9.3 nl l-1 5.1 µg m3 – 8.0 nl l-1 peak concentrations: > 2 µl l-1 soil/root compartment ...
... 6.6 µg m3 – 9.3 nl l-1 5.1 µg m3 – 8.0 nl l-1 peak concentrations: > 2 µl l-1 soil/root compartment ...
Temperature Trends in the Lower Atmosphere: Steps for
... of climate model simulations and the reality of greenhouse gas-induced global warming. As described in the Executive Summary, considerable progress has been made in resolving many of these earlier discrepancies. Background Measurements of global surface air temperature show substantial increases ove ...
... of climate model simulations and the reality of greenhouse gas-induced global warming. As described in the Executive Summary, considerable progress has been made in resolving many of these earlier discrepancies. Background Measurements of global surface air temperature show substantial increases ove ...
Abstract Title of Dissertation: EXPERIMENTAL STUDIES OF
... The experimental arcs matched the cloud-ground (CG) strokes in current waveform, current amplitude and energy dissipation. The current waveform of arcs, primarily determined by an external resistor, agreed well with the overall of CG strokes on the global average. Arc current arrived at its peak fro ...
... The experimental arcs matched the cloud-ground (CG) strokes in current waveform, current amplitude and energy dissipation. The current waveform of arcs, primarily determined by an external resistor, agreed well with the overall of CG strokes on the global average. Arc current arrived at its peak fro ...
The interdependence of continental warm cloud properties derived
... corresponding cumulative probability (solid line) accounted from the larger end of βct,1 km for clear sky at the ARM Oklahoma site in 2005. The dashed line represents the 94 % cumulative probability. ...
... corresponding cumulative probability (solid line) accounted from the larger end of βct,1 km for clear sky at the ARM Oklahoma site in 2005. The dashed line represents the 94 % cumulative probability. ...
Paul Crutzen - Nobel Lecture
... the ozone producing 200-240 nm wavelength region (19, 20). As a result of these developments it became clear that enough NO is produced via reaction R13 to make reactions R11 and R12 the most important ozone loss reactions in the stratosphere in the altitude region between about 25 and 45 km. N 2O i ...
... the ozone producing 200-240 nm wavelength region (19, 20). As a result of these developments it became clear that enough NO is produced via reaction R13 to make reactions R11 and R12 the most important ozone loss reactions in the stratosphere in the altitude region between about 25 and 45 km. N 2O i ...
Week 7 - Ozone Diagrams
... Why has the ozone hole stayed nearly constant for the last 10 years? The short answer is that it’s about as bad as it can get. The size of the ozone hole is largely controlled by atmospheric weather conditions, such as how cold the winter is, and how variable winds are. Even if there was more chlori ...
... Why has the ozone hole stayed nearly constant for the last 10 years? The short answer is that it’s about as bad as it can get. The size of the ozone hole is largely controlled by atmospheric weather conditions, such as how cold the winter is, and how variable winds are. Even if there was more chlori ...
Twenty Questions and Answers About the Ozone Layer
... accumulation of ODSs has slowed and begun to decrease. In response, global ozone depletion is no longer increasing. Now, with continued compliance, we expect substantial recovery of the ozone layer by the late 21st century. The day the Montreal Protocol was agreed upon, 16 September, is now celebrat ...
... accumulation of ODSs has slowed and begun to decrease. In response, global ozone depletion is no longer increasing. Now, with continued compliance, we expect substantial recovery of the ozone layer by the late 21st century. The day the Montreal Protocol was agreed upon, 16 September, is now celebrat ...
Twenty Questions and Answers About the Ozone Layer
... accumulation of ODSs has slowed and begun to decrease. In response, global ozone depletion is no longer increasing. Now, with continued compliance, we expect substantial recovery of the ozone layer by the late 21st century. The day the Montreal Protocol was agreed upon, 16 September, is now celebrat ...
... accumulation of ODSs has slowed and begun to decrease. In response, global ozone depletion is no longer increasing. Now, with continued compliance, we expect substantial recovery of the ozone layer by the late 21st century. The day the Montreal Protocol was agreed upon, 16 September, is now celebrat ...
+ cos - Astronomia
... a , b , c : sides of the spherical triangle = measurements of the central angles ...
... a , b , c : sides of the spherical triangle = measurements of the central angles ...
MERCURY In-flight calibration of the PHEBUS UV instrument and
... Président du Jury Rapporteur Rapporteur Examinateur Examinateur Directeur de Thèse Superviseur ...
... Président du Jury Rapporteur Rapporteur Examinateur Examinateur Directeur de Thèse Superviseur ...
Ozone Layer: Existence and Anthropogenic Depletion
... months are large fractional increases in small values. Biologically, they may not be of great significance. Increases during the spring and summer, although of smaller degree, may be more significant. This increase is occurring when many species are reproducing and the biological effects may therefo ...
... months are large fractional increases in small values. Biologically, they may not be of great significance. Increases during the spring and summer, although of smaller degree, may be more significant. This increase is occurring when many species are reproducing and the biological effects may therefo ...
Optical properties of cirrus clouds in the tropical tropopause region
... 13-15 km altitude range on most of the days and in about 70% of the cases, the cloud top height is above 15 km. The average height of the local tropopause during summer season is about 17.5 km. During the southwest monsoon season, the altitude range of the clouds is between 10 and 17 km and the loca ...
... 13-15 km altitude range on most of the days and in about 70% of the cases, the cloud top height is above 15 km. The average height of the local tropopause during summer season is about 17.5 km. During the southwest monsoon season, the altitude range of the clouds is between 10 and 17 km and the loca ...
Lab for Remote Sensing Hydrology and Spatial Modeling
... Moisture is removed by orographic lift, leaving drier air on the descending, leeward side where a rain shadow is observed. RSLAB-NTU ...
... Moisture is removed by orographic lift, leaving drier air on the descending, leeward side where a rain shadow is observed. RSLAB-NTU ...
Using stellar scintillation for studies of turbulence in the Earth`s
... that have been successfully used for interpretation of scintillation measurements, the smallscale structure of atmospheric irregularities is very complex and still incompletely described. Measurements of the atmospheric microstructure reveal a fairly large number of very strong (positive) temperatur ...
... that have been successfully used for interpretation of scintillation measurements, the smallscale structure of atmospheric irregularities is very complex and still incompletely described. Measurements of the atmospheric microstructure reveal a fairly large number of very strong (positive) temperatur ...
Hydrochloric acid from chlorocarbons: a significant global
... Hydrochloric acid, measured as non-sea-salt chloride (nssCl−), is a ubiquitous component of continental and marine ‘‘background’’ rain, with concentrations ranging between 1.5 and 3.2 meq/l. The potential contribution of HCl to the acid–basic equilibrium ranges from ~10% to ~40%; showing that this a ...
... Hydrochloric acid, measured as non-sea-salt chloride (nssCl−), is a ubiquitous component of continental and marine ‘‘background’’ rain, with concentrations ranging between 1.5 and 3.2 meq/l. The potential contribution of HCl to the acid–basic equilibrium ranges from ~10% to ~40%; showing that this a ...
Isotope constraints on particulate nitrogen source and dynamics in
... (around the SouthEast Asian Time-series Study (SEATS) station) was explored by examining the isotopic compositions of suspended PN in the top 200 m over 3 years and sinking PN collected by sediment traps. The PN inventory (IPN) in the upper 100 m is larger than in the lower 100 m, exhibiting stronge ...
... (around the SouthEast Asian Time-series Study (SEATS) station) was explored by examining the isotopic compositions of suspended PN in the top 200 m over 3 years and sinking PN collected by sediment traps. The PN inventory (IPN) in the upper 100 m is larger than in the lower 100 m, exhibiting stronge ...
Tropospheric Ozone Lesson: Student worksheets
... How do weather conditions affect tropospheric ozone formation? In addition to NOx and VOCs, weather conditions or meteorological factors are known to have some influence in the formation of tropospheric ozone. These factors include temperature, humidity, cloud cover and wind direction and speed. Com ...
... How do weather conditions affect tropospheric ozone formation? In addition to NOx and VOCs, weather conditions or meteorological factors are known to have some influence in the formation of tropospheric ozone. These factors include temperature, humidity, cloud cover and wind direction and speed. Com ...
Nature template - PC Word 97
... contribute to this tropospheric signature, which over millennial time scales might be preserved in ice cores from polar regions in which downwelling air is prevalent (16) Along with a recent three-isotope measurement of O2 in a closed system (30), our understanding of biospheric processes could be f ...
... contribute to this tropospheric signature, which over millennial time scales might be preserved in ice cores from polar regions in which downwelling air is prevalent (16) Along with a recent three-isotope measurement of O2 in a closed system (30), our understanding of biospheric processes could be f ...
The Hydrological Cycle over a Wide Range of
... relatively equable climate, with an equator-to-pole difference in surface air temperature of 31 K (equatorial and polar temperatures of 311 and 280 K, respectively). The extratropical relative humidity in the lower free troposphere decreases as the surface temperature increases, while at upper level ...
... relatively equable climate, with an equator-to-pole difference in surface air temperature of 31 K (equatorial and polar temperatures of 311 and 280 K, respectively). The extratropical relative humidity in the lower free troposphere decreases as the surface temperature increases, while at upper level ...
ultraviolet radiation in the solar system
... window is always followed by an increase in knowledge of the subject concerned. This is also the case with the subject of this book, ultraviolet radiation (hereafter UV). In principle, the ultraviolet range might be just one more of these windows, of no particular importance. However, the energy per ...
... window is always followed by an increase in knowledge of the subject concerned. This is also the case with the subject of this book, ultraviolet radiation (hereafter UV). In principle, the ultraviolet range might be just one more of these windows, of no particular importance. However, the energy per ...