Thermal structure and circulation in Lake Chapala, Mexico

Avalos-Cueva, David; Filonov, Anatoliy; Tereshchenko, Iryna; Monzón, César; Velazquez-Muñoz, Federico

doi:10.4081/jlimnol.2016.1430

Cited by 3 publications

(4 citation statements)

References 15 publications

(16 reference statements)

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“…Lake Chapala is located between Jalisco and Michoacán, Mexico (20° 15' N and 103° 01' W). Lake Chapala is the largest natural lake in Mexico having an average depth of 6 m, with a maximum depth near 11 m [35]. Lake Chapala (Figure 2) covers an area of circa 1161 km 2 ; its length is over 79 km and has a width of circa 28 km.…”

Section: Lake Chapalamentioning

confidence: 99%

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Analysis of Surface Water Areal changes using Remote Sensing Data

Murray¹,

Khaki²

2020

aeer

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Inland water bodies are crucial for supporting human life in various parts of the world. Therefore, it is essential to accurately monitor its spatiotemporal variations for better water management. The main objective of this study is to investigate the application of remote sensing data for quantifying the surface area changes and the impact of climatological variabilities over Lakes Mead and Chapala. Historical time series of monthly surface area dynamics were developed using Landsat 1-8 scenes and the climate variability was analysed using evaporation rate and precipitation. Results show that estimated surface water changes from satellite data agree well with independent data. A significant decline in surface area of about 40% since 2000 was found over the Lake Mead region. The relationship between surface area, precipitation and evaporation indicate that climatological factors have contributed to the lake surface area reduction. Lake Chapala’s surface area, on the other hand, has not fallen significantly despite negative trends in precipitation. It was found that human interactions with the lake are likely the main cause of surface area variations. The information about water surface area variation in this study is valuable for monitoring and characterising the predictability of water availability of the regions.

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Section: Lake Chapalamentioning

confidence: 99%

“…Lake Chapala and water inbound from the Lerma River supply water for industry, drinking water and irrigation. On the riverside of Lake Chapala, considerable tourism, fishing, industrial, and agricultural activities are observed [35].…”

Section: Lake Chapalamentioning

confidence: 99%

Analysis of Surface Water Areal changes using Remote Sensing Data

Murray¹,

Khaki²

2020

aeer

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“…Furthermore, Valle de Bravo larger surface area (18.55 km2) favours wind-induced mixing depths larger than those observed in SAMO Lake, which has a significant smaller surface area (3.7 km2). An extreme example is Chapala Lake (Mexico), where its large surface area (1 112 km2) and shallowness cause a warm polymictic regime (Avalos-Cueva et al, 2016;Lind et al, 1997).…”

Section: Heat Transfermentioning

confidence: 99%

Fast deep water warming of a subtropical crater lake

Cardoso-Mohedano

Sanchez-Cabeza

Ruiz-Fernández

et al. 2019

Science of The Total Environment

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“…In Guadalajara, Jalisco the monthly average air temperature from March to May 1998 was 3-4°C higher than the climatological mean for this same season. The atmospheric relative afternoon humidity decreased from 6 to 8% [14]. Due to the intense dry season, the lake lost more than 1 m of its water level due to evaporation and the excess of water pumped to satisfy water demand from the local industry and population [8].…”

Section: Long-term Fluctuations In the Lake Levelmentioning

confidence: 99%

Climatic Change in a Large Shallow Tropical Lake Chapala, Mexico

Filonov¹,

Tereshchenko²,

Monzón³

et al. 2016

Lake Sciences and Climate Change

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Measurements of temperature, currents and lake level taken in 2005-2014 are analyzed and discussed. We obtained a conceptually new data set on the formation of the thermocline in Lake Chapala. It is showed that the thermocline in the lake occurs only during the daytime, in the top 0.5-1.0-m layer of the water column, whereby the vertical temperature gradient reaches 2.5°C/m within that layer. At night, the top layer is cooled, which causes strong vertical mixing down to the bottom. Moored measurements of temperature and level from Lake Chapala reveal the presence of seiches oscillations with periods of 5.7 and 2.8 hours with amplitudes of 15.4 and 8.1 mm. Temperature measurements on sections across the lake showed that in the northern part of the lake, the water column is warmer that in southern 2-3°C in all seasons. The lake currents were simulated for wet and dry seasons. The model results are in good agreement with the acoustic Doppler current profiler (ADCP) data. The presence of an anticyclone gyre in the central part of the lake in both seasons is detected.

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Thermal structure and circulation in Lake Chapala, Mexico

Abstract: This study analyzed and discussed the instrumental measurements of temperature and currents made on January 10, 2007,

Cited by 3 publications

References 15 publications

Analysis of Surface Water Areal changes using Remote Sensing Data

Analysis of Surface Water Areal changes using Remote Sensing Data

Fast deep water warming of a subtropical crater lake

Climatic Change in a Large Shallow Tropical Lake Chapala, Mexico

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