The Water Cycle (AQA A Level Geography): Exam Questions

Exam code: 7037

4 hours24 questions
1
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4 marks

Explain the concept of dynamic equilibrium in relation to the water cycle.

2
4 marks

Outline flows within the water cycle operating on a hill slope.

3
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4 marks

Explain the role of cryospheric change in the water cycle.

4
4 marks

Outline how the magnitude of water stores within the hydrological cycle can change.

5
4 marks

Outline the processes involved in generating overland flow in a drainage basin.

6
4 marks

Outline the role of vegetation in the water cycle

7
4 marks

Outline how human factors impact upon the water cycle.

8
4 marks

Outline the purpose of a flood hydrograph.

1
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6 marks

Figure 1 represents data from a climate model for Africa. The map shows how rainfall totals are expected to change in Africa by 2099 compared with 1986−2005 averages. The graphs show predictions for rainfall change by month between 2080 and 2099, compared with average rainfall taken from 1986−2005.

Figure 1

fig-1-paper1-specimen-aqa-alevel-geography

Using Figure 1, analyse projected rainfall change in Africa.

2
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6 marks

Using Figure 2 and your own knowledge, assess the natural and human-induced causes of the 2005 flood in Carlisle.

Figure 2

There were two separate aspects within this period of storm which affected the River Eden drainage basin around the city of Carlisle, England. Three rivers converge in the city, which has a population of approximately 72 000. There had been several weeks of above average rainfall for January. The January 2005 flood was a major event. Rainfall was very high for the period 6 to 8 January, during which two months’ worth of rainfall was released in 24 hours. Some areas within the catchment received rainfall of up to 150 mm.

The upper parts of the catchment are dominated by the mountains of Skiddaw and the surrounding fells. The rocks here are hard and volcanic, soils are thin, and the gradients of many tributaries are steep. In the lower reaches rivers flow through wide, shallow valleys.

The Eden channel itself has a steep gradient. The head of the catchment is around 690 m, falling rapidly to 160 m. The Eden's glaciated valley opens out and the channel gradient reflects this change: the River Eden steadily loses height at around 1.8 m per km on its journey to Carlisle. The valley floor is over 2.5 km wide in many places. This forms extensive areas of floodplain.

In terms of land use, the drainage basin has a wide range of agricultural activity, both arable and pastoral farming. There are also golf courses and a small amount of managed forestry. As the River Eden reaches the coast, the area to the south is the heavily developed city of Carlisle. Much of the area is rural apart from this. 67% of the flooding resulted from rivers and watercourses. 25% of flooding was caused by surface water. 8% was due to flooding from sewerage and infrastructure

In Carlisle, the River Eden peaked at an estimated 1520 cumecs at the Sheepmount Gauging Station at 2.30 pm on 8 January. This flow has a return period in the order of 175–200 years (0.5%). The previous highest recorded flow on the River Eden at Carlisle was 1075 cumecs in 1987.

3
6 marks

Figure 1 shows annual and 5-year moving average rainfall data for two measuring stations in South Africa: Royal Observatory and Dwarsberg.

Graph of annual and 5-year moving average rainfall at Dwarsberg and Royal Observatory from 1945-2015, showing fluctuating trends over time.
Annual and 5-year moving average rainfall data for two measuring stations in South Africa: Royal Observatory and Dwarsberg

Note: The 5-year moving average plots the mean value of the previous 5 years.

Analyse the data shown in Figure 1.

4
6 marks

Figure 1 shows the number of days when precipitation is high enough for plant growth across southern Africa in 2000 and that projected for 2050.

Maps of South Africa show the number of days when precipitation is high enough for plant growth in 2000 versus 2050
Maps showing number of days when precipitation is high enough for plant growth in South Africa 2000/2050

Using Figure 1 and your own knowledge, assess the predicted impact of climate change upon life in this region.

5
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6 marks

Figure 2a shows two maps indicating the changing vegetation cover in the Taguibo Watershed in Agusan del Norte province, northeastern Mindanao Island, Philippines, from 1976 and 2001. The third map shows how the area could be rehabilitated with natural vegetation.

Figure 2b shows the possible impact of a storm in 2007 upon the runoff volume in the Taguibo Watershed for each of the situations shown in Figure 2a.

Figure 2a

Changing vegetation cover in the Taguibo Watershed, from 1976 to 2001 and how the area could be rehabilitated with natural vegetation

fig-2a-inserts-paper1-june2019-aqa-alevel-geography

Figure 2b

Possible impact of a storm in 2007 on runoff volume in the Taguibo Watershed for each situation shown in Figure 2a

fig-2b-inserts-paper1-june2019-aqa-alevel-geography

Using Figure 2a, Figure 2b and your own knowledge, assess the potential impact of changing vegetation cover upon runoff in this area.

6
6 marks

Figure X shows rainfall data, a measured hydrograph and a simulated hydrograph for Taguibo Watershed in Mindanao Island, southern Philippines. The data were collected from 13 to 17 April 2007. The simulated hydrograph is a computer-generated prediction of discharge.

Graph showing discharge (m³/s) and rainfall (mm/10 min) over time. Measured hydrograph in red, simulated in black, rainfall in blue bars. Dates: 14-17 April 2007.

Analyse the data shown in Figure X.

[6]

7
6 marks

Analyse the data shown in Table 1 on water balance components for selected UK river catchments.

Table 1: Mean annual water balance components for selected UK river catchments (2020–2022 average)

Catchment

Annual precipitation (mm)

Potential evapotranspiration (mm)

Surface runoff (mm)

Groundwater recharge (mm)

River Exe (SW England)

1,650

520

890

240

River Thames (SE England)

680

490

120

70

River Severn (Wales/W England)

1,200

480

580

140

River Eden (NW England)

1,980

440

1,350

190

River Lee (SE England)

640

510

80

50

Source: Environment Agency / Centre for Ecology and Hydrology (2023)

8
6 marks

Analyse the data shown in Figure 1.

Figure 1: River discharge and hourly rainfall data for the River Eden at Carlisle during a storm event, December 2015.

Time (hours from storm onset)

Hourly rainfall (mm/hr)

River discharge (m³/s)

0

5

280

3

12

295

6

25

380

9

35

590

12

40

860

15

38

1,150

18

20

1,480

21

8

1,510

24

3

1,390

30

0

1,020

36

0

720

48

0

450

Source: Adapted from Environment Agency discharge records, River Eden at Carlisle, December 2015.

9
6 marks

Using Figure 2 and your own knowledge, assess the factors affecting infiltration rates in a drainage basin.

Figure 2: A line graph showing infiltration rates over time for three contrasting land surface types in a temperate UK drainage basin.

Line graph of infiltration rates over 120 minutes, showing woodland highest and declining, moorland moderate, and urban surface lowest with little change.

Source: Adapted from Environment Agency natural flood management research data, 2018.

10
6 marks

Figure 2 shows river flow data measured at various gauging stations across parts of the UK on 7 November 2019.

River flow data measured at various gauging stations across parts of the UK on 7 November 2019.

Using Figure 2 and your own knowledge, assess factors affecting the likelihood of flooding across the UK.

1
20 marks

With reference to a river catchment that you have studied, assess the potential factors that could impact the flood hydrograph.

2
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20 marks

Assess the potential causes and impacts of changes to the water balance within a tropical rainforest that you have studied.

3
20 marks

Assess the extent to which human activity has changed the water cycle.

4
20 marks

Evaluate the factors that cause variations in drainage basin runoff.

5
20 marks

Evaluate the factors responsible for changes in the magnitude of water stores over time.

6
20 marks

Evaluate the extent to which human activities have disturbed the global water cycle.