The count of the number of high points of a wave passing point \"X\" over time \
ID: 292842 • Letter: T
Question
The count of the number of high points of a wave passing point "X" over time "Y" is ___________________.
In what pattern does sediment move down-coast in the longshore current?
This is the term for waves caused by direct wind stress.
Which is saltier?
Which processes can decrease ocean salinity? (Select all that apply.)
What is the effect of adding CO2 to seawater?
wave height Quescion 45 wae height Question 46 n whuf. pattem does secinmernt mn dow cost inChe longshore urret Strzlght Ine parallel to shere o Otitz ?Streight lnepe pernScula' to s.oe Question 47 This is the term or waes caused by direct wind stress Translztion Stoss Question 48 Which s sade? ?Brackish vater O Erine Seavater O Sine Question 19 Whith pecesses can decrease ocean salnity? elect all thaapph:) Precipitation Question 50 what s the erfect ? adcing CO2tasea water? Retres its densityExplanation / Answer
1) wave frequency
frequency is the number of complete cycles per second, or the number of high points of a wave passes in a unit time.
2) zig zag
long shore drift is a geological process which involves sediment transportation, along the coast and parallel to the shore line, most of the beach sand move to down beach in a zig zag manner with a speed of tens of meters per day.
3) swell
swell is the mechanical wave produced in the lakes and oceans generated by the interaction of water and wind, so this is also known as surface gravity waves.
4)brine
brine is the high concentration solution of salt usually sodium chloride,it can range from 3.5 to 26% , it can be formed by the high evaporation rate, brine is naturally occurs on earths surface as salt lake on land and brine pools on ocean bottom.
5) melting of ice and precipitation.
these two process decrease the salinity of ocean by adding fresh water to the saline water, but in the case of evaporation it increases the salinity by reducing the water level and during freezing of sea water, salt will left over this will incease salinity around the ice formations.
6) Lower its PH
this process is known as ocean acidification, by the intake of cabon dioxide from atmoshere, PH of the ocean water deacreases from slightly basic to neutral.
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