or is it just me? Ice in the Hole Miyamoto Monument End of the Tunnel A Path in the Clouds A Mysterious House of Ice The Escape Icy Valley The Shattered Bridge Arctic ruins Over the Frozen Bridge The Castle of Nolok No More Mr. Combining warm and cold nonprecipitating clouds gives a global ratio of IWP to LWP that is about 0.7 over oceans.Full Game Leaderboard Category Extensions Level Leaderboard All Welcome to Antarctica The Journey Begins Via Nostalgica Tobgle Road A Fork in the Road The Somewhat Smaller Bath The Frosted Fields Oh no! More Snowballs! Stone Cold Grumbel's Sense of Snow 23rd Airborne Night Chill Into the Stars Above the Arctic Skies Entrance to the cave Under the Ice Living in a Fridge. The ratio of IWP to LWP in cold nonprecipitating clouds reaches almost 3 in the northern midlatitudes in autumn and falls as low as 0.6 in the southern midlatitudes in spring–summer. Ice fractions, IWP/(LWP + IWP), in cold nonprecipitating clouds increase systematically with decreasing cloud-top temperatures, reaching 50% at about – 15☌ but ranging from about −5° to −10☌ in the northern midlatitudes in autumn and the Tropics year-round to about −25☌ in the southern midlatitudes in summer. Tropical and cold hemisphere clouds have higher IWP values (around 10 mg cm−2) than those in warm hemispheres whereas LWP values for warm nonprecipitating clouds vary little with latitude or season. The average IWP for cold nonprecipitating clouds is about 7 mg cm−2, with LWP being about 5 mg cm−2. The values of total water path obtained from the ISCCP values of optical thickness for cold nonprecipitating clouds are larger than the LWP values from SSM/I, which the authors explain in terms of IWP. The average IWP for cold nonprecipitating clouds is about 7 mg cm-2, with LWP being about 5 mg cm-2. The average LWP for warm nonprecipitating clouds is about 6 mg cm−2. The values of total water path obtained from the ISCCP values of optical thickness for cold nonprecipitating clouds are larger than the LWP values from SSM/I, which the authors explain in terms of IWP. About 93% of all clouds are nonprecipitating clouds, and about half of nonprecipitating clouds are warm (cloud-top temperature > 0☌). SSM/I data are used to separate precipitating and nonprecipitating clouds and to determine LWP. CErrorHandler CExplosion, Just your average explosion - goes boom, hurts Tux CExposedObject, This class binds a certain GameObject class to a scripting class. The ISCCP data are used to separate clear/cloudy skies and warm/cold clouds and to determine cloud optical thickness, cloud-top temperature, and sea surface temperature. Seasonal variations of liquid and ice water paths (LWP and IWP) in nonprecipitating clouds over oceans are estimated for 4 months by combining the International Satellite Cloud Climatology Project (ISCCP) and Special Sensor Microwave/Imager (SSM/I) data.
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