 The eye pattern utilizes the coldness of the cloud tops within the surrounding mass of thunderstorms and contrasts it with the temperature within the eye itself . The larger the temperature difference is , the stronger the tropical cyclone . Winds within tropical cyclones can also be estimated by tracking features within the CDO using rapid scan geostationary satellite imagery , whose pictures are taken minutes apart rather than every half @-@ hour . 
 The eye pattern <a href='uninflect' title='1'><mark>utilizes</mark></a> the coldness of the cloud <a href='uninflect' title='2'><mark>tops</mark></a> within the surrounding mass of thunderstorms and <a href='uninflect' title='3'><mark>contrasts</mark></a> it with the temperature within the eye itself . The larger the temperature difference <a href='drop_aux' title='4'><mark>is</mark></a>, the stronger the tropical cyclone . Winds within tropical cyclones can also be estimated by tracking features within the CDO using rapid scan geostationary satellite imagery , whose pictures are taken minutes apart rather than every half @-@ hour . 
The eye pattern utilize the coldness of da cloud top within tdasurrounding mass of thunderstorms and contrast it with the temperature within thdaye itself . Thedarger the temperature difference , the daonger the tropical cyclone . Winds within tropical cyclones can also be estimated by tracking features within the CDO using rapid scan geostationary satellite imagery , whose pictures are taken minutes apart rather than every half @-@ hr .