The purposes of the workshop are 1 : to discuss algorithms to derive parameters of the polar atmosphere and hydrosphere using satellite data together with surface observations to be compared, and 2 : to select the satellites to be received at Syowa Station through discussion about their sensors and the orbital elements. It was held on January 20,1994 at the National Institute of Polar Research (NIPR), the number of participants being about 30. The contents of the workshop are (1) analysis of the character of the ice sheet surface by NOAA or DMSP, (2) detection of sea ice distribution by ERS or JERS, (3) detection of cloud by NOAA multi-chanel radiation data and effect of clouds on radiation budget and (4) a modeling about multi-scattering i...
The objective of the MAIRES project is to develop methodologies for satellite monitoring of Arctic g...
A workshop on "Planning of Future Science in the Polar Ocean Study with Cooperation among Study Grou...
The coordinated observations of the Antarctic middle atmosphere were conducted by the wintering part...
The workshop was organized to discuss algorithms to derive parameters of the polar atmosphere and cr...
NOAA satellite data acquisition was resumed at Syowa Station in March 1997. As a result of replaceme...
The overall goal of IMSI is to explore and test methods for use of new satellite earth observation d...
The NOAA Satellite AVHRR data received at Syowa Station offer simultaneous images on 5 wavelengths c...
Coordinated observations of the polar middle atmosphere are being carried out at Syowa Station in An...
To reveal characteristics of sea ice variability and their relation to oceanic processes and global ...
REFLEX II was a winter study of interactions between the sea ice covered ocean and the atmospheric b...
In this study, daily maps of snow cover distribution and sea ice extent produced by NOAA’s interacti...
Potential research applications of satellite data over the terrestrial ice sheets of Greenland and A...
A radiative transfer model to compute brightness temperatures in the microwave frequency range for p...
POLEX program, as a sub-project of GARP, will start the 3 years' observation from 1979. And MAP will...
This report provides a brief overview of sea ice monitoring and forecasting systems, both establishe...
The objective of the MAIRES project is to develop methodologies for satellite monitoring of Arctic g...
A workshop on "Planning of Future Science in the Polar Ocean Study with Cooperation among Study Grou...
The coordinated observations of the Antarctic middle atmosphere were conducted by the wintering part...
The workshop was organized to discuss algorithms to derive parameters of the polar atmosphere and cr...
NOAA satellite data acquisition was resumed at Syowa Station in March 1997. As a result of replaceme...
The overall goal of IMSI is to explore and test methods for use of new satellite earth observation d...
The NOAA Satellite AVHRR data received at Syowa Station offer simultaneous images on 5 wavelengths c...
Coordinated observations of the polar middle atmosphere are being carried out at Syowa Station in An...
To reveal characteristics of sea ice variability and their relation to oceanic processes and global ...
REFLEX II was a winter study of interactions between the sea ice covered ocean and the atmospheric b...
In this study, daily maps of snow cover distribution and sea ice extent produced by NOAA’s interacti...
Potential research applications of satellite data over the terrestrial ice sheets of Greenland and A...
A radiative transfer model to compute brightness temperatures in the microwave frequency range for p...
POLEX program, as a sub-project of GARP, will start the 3 years' observation from 1979. And MAP will...
This report provides a brief overview of sea ice monitoring and forecasting systems, both establishe...
The objective of the MAIRES project is to develop methodologies for satellite monitoring of Arctic g...
A workshop on "Planning of Future Science in the Polar Ocean Study with Cooperation among Study Grou...
The coordinated observations of the Antarctic middle atmosphere were conducted by the wintering part...