(আবহাওয়া

Noun:

সমদ্বিবাহু ত্রিভুজ,

isotherms শব্দের বাংলা অর্থ এর উদাহরণ:

আর কেবল দুই বাহু সমান হলে তাকে সমদ্বিবাহু ত্রিভুজ এবং তিনটি বাহুই সমান হলে তাকে সমবাহু ত্রিভুজ বলা হয় ।

একটি চরম সমদ্বিবাহু ত্রিভুজ যার কোণগুলো সোনালি অনুপাতের (Φ:1) বৈশিষ্ট্যযুক্ত ।

সমদ্বিবাহু ত্রিভুজে ।

সমদ্বিবাহু ত্রিভুজ 1 2 b a 2 − b 2 4 = b 4 4 a 2 − b 2 {\displaystyle {\frac {1}{2}}b{\sqrt ।

সমদ্বিবাহু ত্রিভুজের শীর্ষকোণ ।

BCD ত্রিভুজের দুই বাহু সমান, তাই এটি একটি সমদ্বিবাহু ত্রিভুজ ।

সমদ্বিবাহু ত্রিভুজ - যার যে-কোন দুইটি বাহুর দৈর্ঘ্য সমান ।

isotherms's Usage Examples:

diagrams use multiple overlapping contour sets (including isobars and isotherms) to present a picture of the major thermodynamic factors in a weather.

behavior can be properly fit by isotherms with a theoretical basis, it is usually appropriate to use such isotherms instead (see for example the Langmuir.

+ 1 {\displaystyle T_{i+1}} are the color temperatures of the look-up isotherms and i is chosen such that T i < T c < T i + 1 {\displaystyle T_{i}

solutions to measure water vapor sorption isotherms.

The main application of DVS is to measure water sorption isotherms.

Because of the complexity of sorption processes, the isotherms cannot be determined explicitly by calculation, but must be recorded experimentally.

The adsorption of gases and solutes is usually described through isotherms, that is, the amount of adsorbate on the adsorbent as a function of its.

Maps using isotherms show temperature gradients, which can help locate weather fronts.

desert climates" from "cold desert climates", there are three widely used isotherms: most commonly a mean annual temperature of 18 °C (64.

1872, expanded on the work of Thomas Andrews, and included plots of the isotherms of carbon dioxide at high pressures.

with the isotherms in mireds.

Note the even spacing of the isotherms when using the reciprocal temperature scale.

The even spacing of the isotherms on the.

isotherms are concave towards the north-east direction (45°), then adiabats are concave towards the east north-east (31°).

If adiabats and isotherms are.

determine pore size distribution and surface area through adsorption isotherms.

example, "a 3°C change in mean annual temperature corresponds to a shift in isotherms of approximately 300–400 km in latitude (in the temperate zone) or 500.

mid-19th century by using surface weather observations to analyze isobars, isotherms, and display temperature and cloud cover.

the dry adiabats make an angle of about 45 degrees with the isobars, isotherms are vertical and isopleths of saturation mixing ratio are almost straight.

The isotherms are straight and vertical, isobars are straight and horizontal and dry.

allows straight, horizontal isobars and provides for a large angle between isotherms and dry adiabats, similar to that in the tephigram.

isotherms's Meaning':

(meteorology