HYDROMETEOROLOGY (LESSON 2.3A)

Test

Jugadas 5

Crear copia

Sobre esta actividad

EVAPORATION AND EVAPOTRANSPIRATION

Creada por

Grace Balahay

Estados Unidos

Descarga la versión para jugar en papel

Top 10 resultados

#	Jugador	Acierto	tiempo
1	Grace Balahay 11 de Diciembre de 2025	% 93	02:24

¿Quieres aparecer en el Top 10 de este juego? Inicia sesión para identificarte.

Crea tu propio juego gratis desde nuestro creador de juegos

Compite contra tus amigos para ver quien consigue la mejor puntuación en esta actividad

Crear reto

Tipos de sintagmas (II)

idoia rubio

España

(945)

Actividades interactivas para reconocer los distintos tipos de sintagmas
Verbos irregulares en Inglés

Hélmer González Serrano

Colombia

(315)

Se presentan 10 preguntas, cada una con 4 opciones de respuesta. Seleccione la que considere correcta.
Brawl stars preguntas

Carlos Andrés Prieto Rodríguez

Colombia

(165)

Completa todas las preguntas
cuanto sabes de Futbol

hugo estay

Chile

(324)

este test esta basado en las diapositivas que pudimos ver con anterioridad, consta de 10 preguntas las cuales tienen alternativas para poder resolverlas.
Cultura general española

Ernest Serret

España

(101)

Responde las siguientes preguntas


HYDROMETEOROLOGY (LESSON 2.3A)Versión en línea EVAPORATION AND EVAPOTRANSPIRATION por Grace Balahay 1 is the transferal of liquid water into a gaseous state and its diffusion into the atmosphere Written answer 2 evaporation may be a minor component of hydrologic cycle due to little available energy Written answer 3 abundant available energy and has a potential to become part of the water balance Written answer 4 Evaporation is a cooling process in that the latent heat of vaporization (at about ______ of evaporated water) must be provided by the water body Written answer 5 is a function of the differences in vapor pressure at the water surface (ew) and in the atmosphere (actual; ea) Written answer 6 aids in removing the evaporated water vapor from the zone of evaporation and consequently creates greater scope for evaporation. Written answer 7 is a function of the size of the water surface. For large water bodies high-speed turbulent winds are needed to cause maximum rate of evaporation Written answer 8 is the evaporation that occurs above a body of water such as a lake, stream or the oceans. Written answer 9 is that which occurs over the land’s surface, or would occur if the water supply were unrestricted Written answer 10 This occurs when a soil is wet and what evaporation is able to happen occurs without a lack of water supply. Written answer 11 is that which actually occurs (i.e., if there is not much available water it will be less than potential) Written answer 12 are water-containing pans which are exposed to the atmosphere and the loss of water by evaporation measured in them at regular intervals. Written answer 13 • The simplest of the three analytical methods and is also the least reliable • It involves writing the hydrological continuity equation for the lake and determining the evaporation from a knowledge or estimation of other variables • Thus, considering the daily average values for a lake, the continuity equation is written as Written answer 14 • It is an application of the law of conservation of energy. • The energy available for evaporation is determined by considering the incoming energy, outgoing energy and energy stored in the water body over a known time interval. Written answer 15 bases primarily on the concept of the turbulent transfer of water vapor (by eddy motion) from an evaporating surface to the atmosphere. - based on the concepts of discontinuous and continuous mixing at the air-liquid surface Written answer

HYDROMETEOROLOGY (LESSON 2.3A)Versión en línea

EVAPORATION AND EVAPOTRANSPIRATION

por Grace Balahay

is the transferal of liquid water into a gaseous state and its diffusion into the atmosphere

Written answer

evaporation may be a minor component of hydrologic cycle due to little available energy

Written answer

abundant available energy and has a potential to become part of the water balance

Written answer

Evaporation is a cooling process in that the latent heat of vaporization (at about ______ of evaporated water) must be provided by the water body

Written answer

is a function of the differences in vapor pressure at the water surface (ew) and in the atmosphere (actual; ea)

Written answer

aids in removing the evaporated water vapor from the zone of evaporation and consequently creates greater scope for evaporation.

Written answer

is a function of the size of the water surface. For large water bodies high-speed turbulent winds are needed to cause maximum rate of evaporation

Written answer

is the evaporation that occurs above a body of water such as a lake, stream or the oceans.

Written answer

is that which occurs over the land’s surface, or would occur if the water supply were unrestricted

Written answer

This occurs when a soil is wet and what evaporation is able to happen occurs without a lack of water supply.

Written answer

is that which actually occurs (i.e., if there is not much available water it will be less than potential)

Written answer

are water-containing pans which are exposed to the atmosphere and the loss of water by evaporation measured in them at regular intervals.

Written answer

• The simplest of the three analytical methods and is also the least reliable • It involves writing the hydrological continuity equation for the lake and determining the evaporation from a knowledge or estimation of other variables • Thus, considering the daily average values for a lake, the continuity equation is written as

Written answer

• It is an application of the law of conservation of energy. • The energy available for evaporation is determined by considering the incoming energy, outgoing energy and energy stored in the water body over a known time interval.

Written answer

bases primarily on the concept of the turbulent transfer of water vapor (by eddy motion) from an evaporating surface to the atmosphere. - based on the concepts of discontinuous and continuous mixing at the air-liquid surface

		%
	Anónimo	%
		%
		%

HYDROMETEOROLOGY (LESSON 2.3A)

Test

Sobre esta actividad

Creada por

Descarga la versión para jugar en papel

Top juegos

Test

Tipos de sintagmas (II)

Test

Verbos irregulares en Inglés

Test

Brawl stars preguntas

Test

cuanto sabes de Futbol

Test

Cultura general española

HYDROMETEOROLOGY (LESSON 2.3A)Versión en línea

por Grace Balahay

is the transferal of liquid water into a gaseous state and its diffusion into the atmosphere

evaporation may be a minor component of hydrologic cycle due to little available energy

abundant available energy and has a potential to become part of the water balance

Evaporation is a cooling process in that the latent heat of vaporization (at about ______ of evaporated water) must be provided by the water body

is a function of the differences in vapor pressure at the water surface (ew) and in the atmosphere (actual; ea)

aids in removing the evaporated water vapor from the zone of evaporation and consequently creates greater scope for evaporation.

is a function of the size of the water surface. For large water bodies high-speed turbulent winds are needed to cause maximum rate of evaporation

is the evaporation that occurs above a body of water such as a lake, stream or the oceans.

is that which occurs over the land’s surface, or would occur if the water supply were unrestricted

This occurs when a soil is wet and what evaporation is able to happen occurs without a lack of water supply.

is that which actually occurs (i.e., if there is not much available water it will be less than potential)

are water-containing pans which are exposed to the atmosphere and the loss of water by evaporation measured in them at regular intervals.

• It is an application of the law of conservation of energy. • The energy available for evaporation is determined by considering the incoming energy, outgoing energy and energy stored in the water body over a known time interval.

bases primarily on the concept of the turbulent transfer of water vapor (by eddy motion) from an evaporating surface to the atmosphere. - based on the concepts of discontinuous and continuous mixing at the air-liquid surface