The Characteristics And Differences Between Weather And Weather

The climate of the interior plains is continental, which basically means that the climate is relatively dry with extremely hot summers and cold winters. The weather is very diverse and may change quickly without warning. In the North of the physiographic region, the winters are long and the summers are short and cool whereas in the South, the the winters are harsh with little precipitation and long summers. Although the humid weather and the flat lands create an ideal place to grow crops like wheat and corn, the growing season itself is quite short, even in the southern region due to the lack of precipitation needed for diversified crops to flourish. The flat prairies east to the Rockies is a meeting ground for Arctic, Pacific and

The term Climate Change refers to the changes in typical weather patterns for given regions- this

In the north, the climate typically consists of hot and humid summers and mild to very severe winters. These severe winters result in freezing temperatures,

4. Places downwind of a large body of water generally have milder seasons than places farther inland at the same latitude.

There are many climates all over the world. Many climates have similar weather patterns. The Marine West Coast climate and the Humid Continental climate are in different regions. Both of these climates are similar yet different.

2- Air pressure is not usually a constant that’s why usually impacts therefore it usually weather not climate. Some several key areas of the globe have consistent highs and lows that affect the weather and wind patterns having a huge impact on the climate.

Temperatures can vary widely between regions (such as the mountains and valleys), and between seasons.

Surface temperature differences in turn cause pressure differences. A hot surface heats the air above it and the air expands, lowering the air pressure and its density. The resulting horizontal pressure gradient accelerates the air from high to low pressure, creating wind, and Earth's rotation then causes curvature of the flow via the Coriolis effect. The simple systems thus formed can then display emergent behaviour to produce more complex systems and thus other weather phenomena. Large scale examples include the Hadley cell while a smaller scale example would be coastal breezes.

Climate change can be defined as a significant change in the “average weather” of any given region sustained in the long-term and can be caused by Earth 's dynamic processes, external forces including variations in sunlight intensity, and also by human activities (USEPA, 2014).

The climate in this area varies quite a bit due to the different levels of

An air mass is a huge body of air in the lower atmosphere that has similar temperature, humidity, and air pressure at any given height. Four major types of air masses influenced the weather in North America: maritime tropical, continental tropical, maritime polar, and continental. Maritime air masses form over the ocean and can be very humid. Continental air masses form over land and drier than maritime air masses. Tropical air masses are warm, form in the tropics, and have low air pressure. Polar air masses are cold, form near the poles, and have high air pressure in North America, most air masses move from west to east. The jet stream is a band of high-speed wind about 10 km above the surface

I. (Main Point = Need) According to NASA climate is made up of two things. Those two things are the climates of certain locations during the different seasons and the Earth’s climate which is a combination of all those different induvial climates.

The primary cause of climate change is the human expansion of the greenhouse effect. The greenhouse effect is a natural occurrence, which NASA defines as “the warming that results when the atmosphere traps heat radiating from space” (NASA). During the greenhouse effect, heat from the sun passes through the atmosphere, which is made up of various gases. When the heat from the sun reaches the surface, some of it radiates away from Earth, back into space. However, some of the gases in the atmosphere, known as greenhouse gases, absorb this heat, preventing it from escaping (World Meteorological Organization). The greenhouse effect keeps the Earth at a habitable temperature. The World Meteorological Organization, or WMO, states that the greenhouse effect and

Weather is the combination of temperature, humidity, precipitation, cloudiness, visibility, and wind. In popular usage, climate represents the synthesis of weather; more formally it is the weather of a locality averaged over some period (usually 30 years) plus statistics of weather extremes.

New Zealand’s climate can only be described in one word: unpredictable. Though mostly it has cool to warm temperature, it has microclimates, which is a local atmospheric zone where the climate is different from the surrounding area, owing to its varied topography, and mountain ranges. It has rainfall which is evenly distributed throughout the year in most parts of the country but such is still dependent on the area’s topography as some land area are considered to have borderline oceanic climate or a climate that is intermediate between desert and humid. The country also experiences varied snow falls depending on its parts. Its higher altitude commonly receives ample snow fall while its sea level area receives unpredictable to rare snow fall moments. And