Introduction
The climate varies from one region to another, depending on the associated location, topography, and human activities. The environment of a particular area is
an issue of concern because
directly affects flora and fauna and economic activities such as farming, aviation, and human settlement. This essay aims to describe the climatic conditions and seasonal weather patterns of the Gulf Coast Region and how it affects vegetation and the aviation industry. The description will include the region’s physical topography and determines the experienced weather patterns. Wind patterns and their effects on the climate will also be provided. Finally, a table and climatogram will be used to show the summary of the climatic variables.
The Regions climate
The Gulf Coast region is majorly classified as humid subtropical. However, the southwestern tip of Florida has features of a tropical environment. Hot and warm temperature is experienced along the Gulf coast for most parts of the years. The three winter months are often associated with cold weather that has mild temperatures. The region is highly vulnerable to hurricanes, severe thunderstorms, and floods (Horne, 1999). A large portion of the Gulf coast has summer precipitation maximum during July or August. These are the wettest months because of the combination of the regular summer thunderstorms. The thunderstorms are produced by relentless heat and humidity. In some cases, heavy winter and early spring rainfall may also be experienced. This winter is mostly experienced in Texas, Houston, Louisiana, and Alabama (Marsooli, Lin, Emanuel, & Feng, 2019). The central cities such as Southern Florida and south Texas experience a dry winter season, with September being the wettest months. The Tornados mostly occurs in the inland part of the Gulf region.
Physical topography and surface features
The gulf coastline comprises a variety of coastal features. Some of which include the apiaries islands, tidal inlets ad deltas, rivers and river deltas cheniers, marshes bays mangrove forest, among others. Approximately two-thirds of the coastline comprises barriers islands, low lying sandy landforms resulting from lagoons or tidal inlets. The barrier island’s structure and composition differ from one to another because they are mainly made of shifting sand (Smith, Miller, & Sheng, 2017). The rest of the coastline comprises mainland shore that erodes do not have lagoons, bays, or sandy beaches. The floor of the Gulf is comprised of abyssal plains that are made up of a large triangular area. The coastal location of this region has substantial effects on the experienced climate. The coastal areas are mostly colder and weather as compared to the inland areas. The large rivers found in this region have also resulted in microclimates. For example, areas near the Mississippi River experience slightly different weather conditions. The low altitude has also resulted in colder climatic conditions.
The main wind patterns in the region and how these wind patterns affect the seasonal climate of the region
Sea breeze plays a significant role, especially during summertime. The wind generally blows from the south to the southwest. The majority of the Gulf, the wind reaches a minimum at around 4 am followed by a steady increase after 6 am. Winds of less than 3.35 mph often characterize the calm condition. Afternoon, the higher wind speed is experienced with a peak of 7-10 mphs that may last for several hours. Generally, the full effect of the sea breeze is experienced during early afternoon hours. At around this time, the wind shifts its direction typically to the south or south to southeast. This diurnal pattern of the local winds is more prominent along the shore line and is experienced in all three months. The Gulf is naturally warmer due to the prevailing sea breeze winds. The wind brings more tropical air into the Gulf, resulting in warm temperatures. In some cases, the sea’s cold air meets with warmer air on land, resulting in a cold front. The front may result in cumulus clouds (Roshan, Moghbel, & Attia, 2020). In the cases where the air is humid and unstable, it may result in thunderstorms. This explains why cities like Florida are famous for the frequent occurrence of thunderstorms.
Affect of climate the local flora/fauna
Large percentages of flora and fauna are found in areas of specific climatic conditions regarding temperature and precipitation. Any alteration of this climatic condition may cause a change in the structure of the plants and animals found in that area, hence changing the entire ecosystem’s makeup. For example, an increase in the temperature may force some organisms to migrate to colder regions. The climatic variation also affects the lifecycle of most plants and animals. For example, in the Gulf region, when the temperature gets warmer, most plants start to grow and bloom earlier in the spring and can survive longer into the fall (Saintilan et al., 2019). In animals, some move out from their hibernations or migrate to different places with favorable conditions. Changes in the climatic conditions such as prolonged droughts and reduced freshwater inflow into the sea may result in the loss of important habitats such as mangrove forests and coral reefs (Saintilan et al., 2019).
Seasonal flying conditions in the region for all seasons
Winter months are generally characterized by mechanical turbulence originating from intense low levels of winds. The turbulence occurs when the winds blow across the rugged terrain. During warmer months of summer, there is reduced turbulence, the temperatures are warmer, and the thunderstorms are much reduced. This is the most favorable season for the aviation industry. The Winter season is also associated with altostratus and nimbostratus clouds. These clouds have a high volume of water in the form of large droplets. During winter, the clouds cover quite an expansive area, resulting in obstruction of flights (Chen & Wang, 2019).
Weather-related threats to aviation
Prevailing weather conditions is a critical issue when it comes to aviation. However, with accurate information, pilots can efficiently operate around it. The wind shear is among the common weather threats to aviation. Although wind shear occurs at any altitude, it is most dangerous when it occurs at low altitude during takeoff or landing. The wind shear may cause a rapid airspeed loss on the final approach, making the flight uncomfortable, almost bringing it to an abrupt stop. Thunderstorms also pause a severe threat to the aviation industry (Horne, 1999). Thunderstorms result in hails that may occur up to 20 miles away. In some cases, strong downdraft and microburst may from below the hails. It can also result in severe turbulence, especially near convective clouds.