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Displaying 20 speakers out of 20
A. MARSHAK
THREE DIMENSIONAL RADIACTIVE EFFECTS OF CLOUD STRUCTURE IN REMOTE SENSING
B. STEIN
AEROSOL LIDAR
C. CAMY-PEYRET
INFRARED METHODS & TECHNIQUES FOR ATMOSPHERIC SCIENCE - LECTURE 1: REPRESENTATIVE SPACE EXPERIMENTS
INFRARED METHODS & TECHNIQUES FOR ATMOSPHERIC SCIENCE - LECTURE 2: RADIATIVE TRANSFER, MOLECULAR
C. READINGS
THE EARTH OBSERVATION PROGRAMME OF THE EUROPEAN SPACE AGENCY: "THE LIVING PLANET PROGRAMME"
THE EARTH OBSERVATION PROGRAMME OF THE EUROPEAN SPACE AGENCY: "THE CURRENT PROGRAMME"
D. FUSSEN
THE ORA EXPERIMENT
D. LABATE
ELECTRO-OPTICAL SPACE INSTRUMENTS FOR ATMOSPHERIC REMOTE SENSING
E. CLOTHIAUX
GROUND-BASED REMOTE SENSING OF CLOUD PROPERTIES USING MILLIMETER-WAVE RADAR
OBJECTIVE DETERMINATION OF CLOUD HEIGHS & RADAR REFLECTIVE USING A COMBINATION OF ACTIVE REMOTE
VERTICAL DISTRIBUTION OF HYDROMETEORS
G. GIOVANNELLI
INTRODUCTION TO THE DOAS METHODOLOGY APPLIED TO ATMOSPHERIC MINOR GAS MEASUREMENTS
THE APE PROJECT
G.P. GOBBI
STUDYING ATMOSPHERIC AEROSOLS BY LIDAR
H. OELHAF
LIMB EMISSION SPECTROSCOPY
I. KOSTANDINOV
POLARIZATION AND RING EFFECT INFLUENCES UPON STRATOSPHERIC DOAS MEASUREMENTS
K. CHANCE
ATMOSPHERIC SPECTROSCOPY & RADIATIVE TRANSFER
K. PFEILSTICKER
IMPROVEMENTS OF DOAS
M. DE MAZIERE
GROUND-BASED MEASUREMENTS OF STRATOSPHERIC TRACE GASES IN THE PERSPECTIVE OF CLIMATE & ENVIRONMENT
ATMOSPHERIC OBSERVATIONS: SYNERGY BETWEEN GROUND, AIRBORNE & SPACE-BASED MEASUREMENTS
P. BIANCO
REMOTE SENSING WITH SMALL SATELLITE CONSTELLATIONS & FORMATIONS
P. SIMON
OZONE NETWORKS
P. SPERA
SPACEBORNE INSTRUMENTATION FOR ATMOSPHERIC SENSING: ALENIA AEROSPAZIO EXPERIENCE
R. FABBO
THE CSA (THE CENTER FOR AGROMETEOROLOGY)
R. GUZZI
INVERSE METHODS IN ATMOSPHERIC PHYSICS
W. WISOMBE
INTRODUCTION TO THE THEORY OF ATMOSPHERIC RADIACTIVE TRANSFERT
IMPROVED MIE SCATTERING ALGORITHMS - EFFICIENCY FACTORS IN MET SCATTERING
NUMERICALLY STABLE ALGORITHM FOR DISCRETE-ORDINATE-METHOD - RADIACTIVE TRANSFER IN MULTIPLE
THE DELTA-M METHOD: RAPID YET ACCURATE RADIATIVE FLUX CALCULATIONS FOR STRONGLY ASYMMETRIC PHASE