Proje ile ilgili açıklama girilmemiştir.

Proje ile ilgili açıklama girilmemiştir.

Proje ile ilgili açıklama girilmemiştir.

Atmosferin Antarktika Kıtası bölgesinde yüksek zamansal çözünürlüklü olarak izlenmesi için GNSS meteorolojisi ve Güneş fotometresi ile Uydu bazlı(MODIS: Aqua, Terra) tekniklerin birlikte kullanılması amaçlanmıştır. Batı ve Doğu Antarktika'dan eş zamanlı gözlemlerle mekansal çözünürlüğe de katkı sunulması hedeflenmiştir.

Proje ile ilgili açıklama girilmemiştir.

Proje ile ilgili açıklama girilmemiştir.

Proje ile ilgili açıklama girilmemiştir.

Proje ile ilgili açıklama girilmemiştir.

Antarktika Bilimsel Araştırma ve Bilim Üssü kurulması ekspedisyon ve projesi

Proje ile ilgili açıklama girilmemiştir.

Antarktika’ya Bilim Üssü Kurulması Ekspedisyon ve Projesi

The sea ice cover floating on the Polar oceans is sensitive to changes in the Earth’s climate system. Routine monitoring of sea ice is based on satellite remote sensing because of the vast area covered. To correctly interprete satellite remote sensing observations of sea ice independent observations are needed. Such observations are difficult to obtain for various reasons – particularly around Antarctica. This project aims to contribute to the improvement of in-situ observations of sea ice around Antarctica. During the Turkish Polar ship expedition ANT001: TrASE heading for the sea area off the Antarctic Peninsula sea ice observations shall be carried out according to the ASPeCt protocol. These will be supported by autonomous camera observations. Contemporary observations according to the ASPeCt protocol will be combined with these camera observations and subsequently compared to co-located satellite remote sensing data. Such inter-comparison helps improving present-day algorithms to derive, e.g., sea ice concentration, sea ice thickness, and snow depth on sea ice – all parameters which are particularly difficult to retrieve adjacent to the rugged coastline of the Antarctic Peninsula.

The main goal of the gratuation project is to integrate new and existing information and methods to provide European ice services and companies with new and improved products and thereby enhance their ability to serve the growing activities in the Arctic and Antarctic and operate in polar conditions. Background: Snow depth from Passive Microwaves (PMW) potentially underestimated over deformed sea ice, Snow depth from PMW influenced by weather-induced changes in snow properties (density, grain size, wetness, layering), Snow depth from PMW influenced by ice-snow interface flooding and related processes. Goals: 1. Co-locate in-situ, buoy and ASPeCt snow depth data with Active MicroWave (AMW), Passive MicroWave (PMW) and other relevant remote sensing and Numerical Weather Prediction (NWP) model data, 2. Search for key parameters that permit to improve PMW snow depth retrieval e.g. by combination with NWP data and/or AMW data, to quantify influence of mentioned contributing factors to PMW snow depths (deformation, snow parameter changes, flooding), 3. Develop, apply and evaluate improved PMW snow depth algorithm for 2-3 key regions

The sea ice cover floating on the Polar oceans is sensitive to changes in the Earth’s climate system. Routine monitoring of sea ice is based on satellite remote sensing because of the vast area covered. To correctly interprete satellite remote sensing observations of sea ice independent observations are needed. Such observations are difficult to obtain for various reasons – particularly around Antarctica. This project aims to contribute to the improvement of in-situ observations of sea ice around Antarctica. During the Turkish Polar ship expedition ANT001: TrASE heading for the sea area off the Antarctic Peninsula sea ice observations shall be carried out according to the ASPeCt protocol. These will be supported by autonomous camera observations. Contemporary observations according to the ASPeCt protocol will be combined with these camera observations and subsequently compared to co-located satellite remote sensing data. Such inter-comparison helps improving present-day algorithms to derive, e.g., sea ice concentration, sea ice thickness, and snow depth on sea ice – all parameters which are particularly difficult to retrieve adjacent to the rugged coastline of the Antarctic Peninsula.

Antartika Çevre Çalışmaları, modellemesi

The SPICES is developing new methods to retrieve sea ice parameters in order to provide enhanced products for polar operators and prediction systems, specifically addressing extreme and unexpected conditions. Automatic remote sensing products traditionally provide general information on sea ice conditions such as ice extent and concentration. However, for ice charting, tactical navigation and management of offshore activities much more important is to know and avoid hazardous sea ice conditions. In general, sea ice hazards are related to sea ice thickness.