Noun:

নর্দন, হাম্বা, নামাল, নিম্ন স্তর,

Adjective:

নিস্তেজ, অর্বাচীন, শান্ত, নিম্নস্বর, অল্পসংখ্যক, মনমরা, হতাশ, হীন, ইতর, বিনত, সামাজিকভাবে পতিত, সামাজিকভাবে অনুন্নত, আনত, আধুনিক, নীচ, হ্রস্ব, ঢিমা, অগভীর, অপ্রচুর, অপূর্ণ, হীনপদস্থ, খর্ব, মৃদু, খাট, অন্ত্য, অবনত, নাবাল, নিম্নস্থ, অনুন্নত, নরম, অনুচ্চ, নিচু, অল্প, নিম্ন, কম,

Adverb:

হ্রাস পাইয়া, কমিয়া, নিম্নধ্বনিতে, মৃদুস্বরে, বিনতভাবে, হীনভাবে, হীন অবস্থায়, হীন স্থানে, নিচু ভাবে, নিচু অবস্থায়, নিচু স্থানে,

lows's Usage Examples:

Thermal lows form due to localized heating caused by greater sunshine over deserts and.

Berg winds are usually accompanied by coastal lows.

These coastal lows owe their existence to the configuration of the plateau, escarpment.

Mesoscale convective systems can spawn surface lows that are initially warm-core.

15 lows per winter, polar lows also occur in Greenland and the Canadian Arctic.

Polar lows can occur at any time during the year, with summer lows tending.

of cold-core lows.

Cold lows can help spawn cyclones with significant weather impacts, such as polar lows, and Kármán vortices.

Cold lows can lead directly.

Low or LOW or lows, may refer to: Low (surname), listing people surnamed Low Low, Quebec, Canada Low, Utah, United States Lo Wu station (MTR code LOW).

typically in the high 20s to mid-30s °C (80s or 90s °F), while overnight lows in the summer are typically in the lower 20s °C (70s °F).

Australian east coast lows (known locally as east coast lows and sometimes as east coast cyclones) are extratropical.

Australian east coast lows (known locally as east coast lows and sometimes as east coast cyclones) are extratropical cyclones.

Tropical lows are the lowest classification on the Australian tropical cyclone intensity scale.

Thermal lows, or heat lows, are non-frontal low-pressure areas that occur over the continents in the subtropics during the warm season, as the result of.

atmosphere leads the lows to the northeast and north-northeast, ("Zugstrasse Vb" Van Bebber) towards the Vienna Basin.

The lows then glide over colder.

Anticyclones aloft can form within warm-core lows such as tropical cyclones, due to descending cool air from the backside of.

winter/colder months than in the summer/warmer months, when the belt of lows and storms generally moves into southern Canada.

When upper cold lows break off from their base, they tend to retrograde and force the development.

recrystallization that drive the movement, this movement then causes topographic lows and valleys to form after all of the material in the ice sheet has been discharged.

After recovering from lows reached following the September 11 attacks, indices slid steadily starting.

Synonyms:

devalued; degraded; grade; depressed; low-level; level; degree; inferior; down; rock-bottom; reduced; debased;

Antonyms:

upward; upwardly; ascending; high; superior;