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THE REGIONAL DIFFERENCES OF GPP ESTIMATION BY SOLAR INDUCED FLUORESCENCE
Gross primary productivity Solar-induced chlorophyll fluorescence, Temperature Precipitation Simple linear regression analysis Determination coefficient
2018/5/15
Estimating gross primary productivity (GPP) at large spatial scales is important for studying the global carbon cycle and global climate change. In this study, the relationship between solar-induced c...
Simultaneous HONO measurements in and above a forest canopy: influence of turbulent exchange on mixing ratio differences
HONO measurements a forest canopy turbulent exchange ratio differences
2011/2/24
We have combined chemical and micrometeorological measurements to investigate the formation and distribution of HONO throughout a forest canopy. HONO was measured simultaneously at two heights, close ...
Exploring the differences in cloud properties observed by the Terra and Aqua MODIS Sensors
cloud properties Terra Aqua MODIS Sensors
2009/6/2
The aerosol-cloud interaction in different parts of the globe is examined here using multi-year statistics of remotely sensed data from two MODIS sensors aboard NASA's Terra (morning) and Aqua (aftern...
Differences across the ITCZ in the chemical characteristics of the Indian Ocean MBL aerosol during INDOEX
ITCZ chemical characteristics Indian Ocean MBL aerosol INDOEX
2009/3/10
The water soluble inorganic part of the sub-micrometer aerosol was measured from two research vessels over the Indian Ocean during the winter monsoon season (February and March) as part of the INDOEX ...
Using GOME NO2 satellite data to examine regional differences in TOMCAT model performance
GOME NO2 satellite data TOMCAT model performance
2009/3/6
This paper compares column measurements of NO2 made by the GOME instrument on ERS-2 to model results from the TOMCAT global CTM. The overall correlation between the model and observations is good (0.7...
Differences in Arctic and Antarctic PSC occurrence as observed by lidar in Ny-Ålesund（79° N, 12° E）and McMurdo（78° S, 167° E）
Arctic Antarctic PSC lidar Ny-Å lesund McMurdo
2009/2/16
The extent of springtime Arctic ozone loss does not reach Antarctic ``ozone hole'' dimensions because of the generally higher temperatures in the northern hemisphere vortex and consequent less polar s...
Differences between ground Dobson, Brewer and satellite TOMS-8, GOME-WFDOAS total ozone observations at Hradec Kralove, Czech
ground Dobson Brewer satellite TOMS-8 GOME-WFDOAS total ozone observations Hradec Kralove Czech
2009/1/19
This paper presents key results achieved by an analysis of the relation between high-quality simultaneous Dobson, Brewer ground and TOMS-V8, GOME-WFDOAS satellite total ozone observations for Hradec K...
Sensitivity of stratospheric inorganic chlorine to differences in transport
stratospheric inorganic chlorine transport
2008/12/19
Correctly modeling stratospheric inorganic chlorine (Cly) is crucial for modeling the past and future evolution of stratospheric ozone. However, comparisons of the chemistry climate models used in the...
Differences between the QBO in the first and in the second half of the ERA-40 reanalysis
QBO ERA-40
2008/12/1
The representation of the quasi-biennial oscillation (QBO) is investigated in the ERA-40 reanalysis. In the lower stratosphere, where there are a reasonable number of observations, the representation ...
Can we reconcile differences in estimates of carbon fluxes from land-use change and forestry for the 1990s
carbon fluxes land-use change forestry
2008/11/11
The effect of Land Use Change and Forestry (LUCF) on terrestrial carbon fluxes can be regarded as a carbon credit or debit under the UNFCCC, but scientific uncertainty in the estimates for LUCF remain...
