Answer : C
reason : give tia ymca eric just
When dealing with the degree of cyclones we have to consider the place where a cyclone can occur.
<h3>Why does a Grade 1 cyclone have more consequences?</h3>
This is due not only to the degree of the cyclone but where it occurs, so a cyclone of degree 1 in a city will have infinitely greater consequences than a hurricane of 5 in the middle of the ocean.
See more about cyclone at brainly.com/question/10412353
Answer:
Explained
Explanation:
three environmental factors that influence food production are:-
1. Climate: food production is directly linked with climate of the place, under different climates different kind of crops are grown. Wheat needs proper sunlight, whereas rice needs plenty of water, it means it grown at places where falls are plenty. Cotton requires temperate climate, it cannot grown in cold regions.
2. Soil: The soil Texture and soil also plays a vital role in crop production. Some soil are less fertile and some are more. Some soil are good for one kind of crop while other is good for other kind of soil. India the Regur or black soil is best for cotton production whereas alluvial soil is best for wheat production. Similarly, laterite soil is best for coffee production.
3. Geographical location and regional variation: Location of the crop field also influences the crop production, some places are good only for a particular crop because of its unique soil. Moreover, the altitude of the places also effects the kind of crop. Generally higher altitude places are colder for example in India Apples are grown only in Parts of Himachal and Kashmir because they are high altitude places making it favorable for Apple
By regulating the amount of water exchange at the Indian-Atlantic Ocean Gateway, or so-called Agulhas Leakage, the meridional variability of the Subtropical Front (STF) in the Southern Hemisphere, linked to expansions or contractions of the Southern Ocean, may have played a significant role in global ocean circulation.
Here, we present new data on primary productivity (chlorins and alkenones) and upper water column temperature (urn:x-wiley:25724517:media:palo21061:palo21061-math-0001 and urn:x-wiley:25724517:media:palo21061:palo21061-math-0002) from marine sediments at IODP Site U1475 on the Agulhas Plateau, close to the In order to analyze indicated changes in the upper oceanic conditions at the mid-Pleistocene transition, we employ these multiproxy time-series records from 1.4 to 0.3 Ma (MPT, ca. 1.2–0.8 Ma).
Our reconstructions in conjunction with earlier proof of the species' migrations of the STF throughout the past 350 ka, the STF may have been farther south from the Agulhas Plateau during the mid-Pleistocene Interim State (MPIS, MIS 23–12), and it may have reached its northernmost position during MIS 34–24 and MIS 10 in the southwest Indian Ocean.
Only the most severe northward migrations of the STF are thought to be related to reduced Agulhas Leakage, according to a comparison with an Agulhas Leakage model obtained from the Cape Basin using Globorotalia menardii.
We believe that the patterns seen during the MPIS may be caused by previously modelled changing westerly winds since STF migrations do not seem to affect Agulhas Leakage variability. In addition to bringing up shifting westerly winds, a separation between STF migrations and Agulhas Leakage may also assist explain fluctuations in CO2 ventilation witnessed throughout the MPIS.
Learn more about STF here:
brainly.com/question/24297407
#SPJ4
